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Subduction zone processes and crustal growth mechanisms at Pacific Rim convergent margins: modern and ancient analogues

Published online by Cambridge University Press:  11 December 2020

Yildirim Dilek Open the ORCID record for Yildirim Dilek [Opens in a new window]  and
Yujiro Ogawa Open the ORCID record for Yujiro Ogawa [Opens in a new window]
Yildirim Dilek*
Affiliation:
Department of Geology & Environmental Earth Science, Miami University, Oxford, OH45056, United States of America
Yujiro Ogawa
Affiliation:
Earth Evolution Sciences, University of Tsukuba, 1-1-1, Tennodai, Tsukuba, Ibaraki, 305-8572Japan
*
Author for correspondence: Yildirim Dilek, Email: [email protected]
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Abstract

Continents grow mainly through magmatism, relamination, accretionary prism development, sediment underplating, tectonic accretion of seamounts, oceanic plateaus and oceanic lithosphere, and collisions of island arcs at convergent margins. The modern Pacific–Rim subduction zone environments present a natural laboratory to examine the nature of these processes. The papers in this special issue focus on the: (1) modern and ancient accretionary margins of Japan; (2) arc–continent collision zone in the Taiwan orogenic belt; (3) accreting versus non-accreting convergent margins of the Americas; and (4) several examples of ancient convergent margins of East Asia. Subduction erosion and sediment underplating are important processes, affecting the melt evolution of arc magmas by giving them special crustal isotopic characteristics. Oblique arc–continent collisions cause strong deformation partitioning that results in orogen-parallel extension, crustal exhumation and wrench faulting in the hinterland, and thrust faulting–folding in the foreland. Trench-parallel widths of subducting slabs exert major control on slab geometries, the degree of coupling–decoupling between the lower and upper plates, and subduction velocity partitioning. An initially large width of the subducting Palaeo-Pacific Plate against East Asia caused flat subduction and resistance to slab rollback during the Triassic Period. These conditions resulted in shortening across SE China. Foundering and delamination of the flat slab during the Early Jurassic Epoch led to slab segmentation and reduced slab widths, followed by slab steepening and rollback. This pull-away tectonics induced lithospheric extension and magmatism in SE China during Late Jurassic – Cretaceous time. Melting of subducted carbonaceous sediments commonly produces networks of silicate veins in CLM that may subsequently undergo partial melting, producing ultrapotassic magmas.

Keywords

Accreting v. non-accreting convergent marginssubduction underplating v. subduction erosionflat subductionslab rollback and extensional tectonicsnear-trench magmatism in accretionary complexesseamount subductionoblique arc–continent collision and strain partitioningultrapotassic magmatism in continental back-arc settings
Type
Original Article
Information
Geological Magazine , Volume 158 , Special Issue 1: Subduction zone processes and crustal growth mechanisms at Pacific-Rim continental margins: modern and ancient analogues , January 2021 , pp. 1 - 12
Copyright
© The Author(s), 2020. Published by Cambridge University Press

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References

Alvarado, D, DeMets, C, Tikoff, B, Hernández, D, Wawrzyniec, TF, Pullinger, C, Mattioli, G, Turner, HL, Rodriguez, M and Correa-Mora, F (2011) Forearc motion and deformation between El Salvador and Nicaragua: GPS, seismic, structural, and paleomagnetic observation. Lithosphere 3, 3–21.CrossRefGoogle Scholar
Anma, R, Armstrong, R, Orihashi, Y, Ike, S-I, Shin, K-C, Kon, Y, Komiya, T, Ota, T, Kagashima, S-I, Shibuya, T, Yamamato, S, Veleso, E, Fanning, EE, Fanning, C and Herve, F (2009) Are the Taitao granites formed due to subduction of the Chile Ridge? Lithos 113, 246–58.10.1016/j.lithos.2009.05.018CrossRefGoogle Scholar
Ayuso, RA, Haeussler, PJ, Bradley, DC, Farris, DW, Foley, NK and Wandless, GA (2009) The role of ridge subduction in determining the geochemistry and Nd–Sr–Pb isotopic evolution of the Kodiak batholith in southern Alaska. Tectonophysics 464, 137–63.10.1016/j.tecto.2008.09.029CrossRefGoogle Scholar
Bassett, D, Sutherland, R, Henrys, S, Stern, T, Scherwath, M, Benson, A, Toulmin, S and Henderson, M (2010) Three-dimensional velocity structure of the northern Hikurangi margin, Raukumara, New Zealand: implications for the growth of continental crust by subduction erosion and tectonic underplating. Geochemistry, Geophysics, Geosystems 11, doi: 10.1029/2010GC003137.CrossRefGoogle Scholar
Brandon, MT and Calderwood, AR (1990) High-pressure metamorphism and uplift of the Olympic subduction complex. Geology 18, 1252–55.2.3.CO;2>CrossRefGoogle Scholar
Brandon, MT, Roden-Tice, MK and Garver, JI (1998) Late Cenozoic exhumation of the Cascadia accretionary wedge in the Olympic Mountains, northwest Washington State. Bulletin of the Geological Society of America 110, 985–1009.2.3.CO;2>CrossRefGoogle Scholar
Brown, M (1998) Ridge-trench interactions and high-T – low-P metamorphism, with particular reference to the Cretaceous evolution of the Japanese Islands. In What Drives Metamorphism and Metamorphic Reactions? (eds Treloar, PJ and O’Brien, PJ), pp. 137–16. Geological Society of London, Special Publication no. 138.Google Scholar
Brown, M (2010) Paired metamorphic belts revisited. Gondwana Research 18, 46–59.CrossRefGoogle Scholar
Brown, D and Ryan, PD (2010) Arc–Continent Collision. Frontiers in Earth Sciences. Volume 4. Berlin, Heidelberg: Springer-Verlag, 493 pp.Google Scholar
Byrne, T, Chan, Y-C, Rau, R-J, Lu, C-Y, Lee, Y-H and Wang, Y-J (2011) The arc–continent collision in Taiwan. In Arc-Continent Collision, Frontiers in Earth Sciences (eds Brown, D and Ryan, PD). Berlin, Heidelberg: Springer-Verlag, doi: 10.1007/978-3-540-88558-0_8.Google Scholar
Calvert, AJ, Preston, LA and Farahbod, AM (2011) Sedimentary underplating at the Cascadia mantle-wedge corner revealed by seismic imaging. Nature Geoscience 4, 545–48, doi: 10.1038/NGEO1195.CrossRefGoogle Scholar
Cawood, P, Kröner, A, Collins, WJ, Kusky, TM, Mooney, W and Windley, BF (2009) Accretionary orogens through Earth history: In Earth Accretionary Systems in Space and Time (eds Cawood, PA and Kröner, A), pp. 1–36. Geological Society of London, Special Publication no. 318, doi: 10.1144/SP318.1.Google Scholar
Chen, WH, Huang, CY, Yan, Y, Dilek, Y, Chen, DF, Wang, MH, Zhang, XC, Lan, Q and Yu, MM (2017) Stratigraphy and provenance of forearc sequences in the Lichi Mélange, Coastal Range: geological records of the active Taiwan arc-continent collision. Journal of Geophysical Research - Solid Earth 122, 7408–36, doi: 10.1002/2017JB014378.CrossRefGoogle Scholar
Clift, PD, Chan, L-H, Blusztajn, J, Layne, GD, Kastner, M and Kelly, RK (2005) Pulsed subduction accretion and tectonic erosion reconstructed since 2.5 Ma from the tephra record offshore Costa Rica. Geochemistry, Geophysics, Geosystems 6, Q09016, doi: 10.1029/2005GC000963.CrossRefGoogle Scholar
Clift, PD and Hartley, AJ (2007) Slow rates of subduction erosion and coastal underplating along the Andean margin of Chile and Peru. Geology 35, 503–06.10.1130/G23584A.1CrossRefGoogle Scholar
Clift, PD and Vannucchi, P (2004) Controls on tectonic accretion versus erosion in subduction zones: implications for the origin and recycling of the continental crust. Reviews of Geophysics 42, RG2001, doi: 10.1029/2003RG000127.CrossRefGoogle Scholar
Clift, PD, Vannucchi, P and Phipps Morgan, J (2009) Crustal redistribution, crust-mantle recycling and Phanerozoic evolution of the continental crust. Earth Science Reviews 97, 80–104, doi: 10.1016/j.earscirev.2009.10.003.CrossRefGoogle Scholar
Cloos, M and Shreve, RL (1988) Subduction-channel model of prism accretion, mélange formation, sediment subduction, and subduction erosion at convergent plate margins: 1. Background and description. Pure and Applied Geophysics 128, 455–500.CrossRefGoogle Scholar
Clowes, RM, Brandon, M, Green, AG, Yorath, CJ, Brown, AS, Kanasewich, ER and Spencer, C (1987) LITHOPROBE - South Vancouver Island: Cenozoic subduction complex imaged by deep seismic reflections. Canadian Journal of Earth Sciences 24, 31–51, doi: 10.1139/e87-004.CrossRefGoogle Scholar
Cole, RB and Basu, AR (1995) Nd-Sr isotopic geochemistry and tectonics of ridge subduction and middle Cenozoic volcanism in western California. Geological Society of America Bulletin 107, 167–79.10.1130/0016-7606(1995)107<0167:NSIGAT>2.3.CO;22.3.CO;2>CrossRefGoogle Scholar
Collins, WJ, Belousova, EA, Kemp, AIS and Murphy, JB (2011) Two contrasting Phanerozoic orogenic systems revealed by hafnium isotope data. Nature Geosciences 4, 333–37, doi: 10.1038/ngeo1127.CrossRefGoogle Scholar
Conticelli, S, Avanzinelli, R, Ammannati, E and Casalini, M (2015) The role of carbon from recycled sediments in the origin of ultrapotassic igneous rocks in the Central Mediterranean. Lithos 232, 174–96.CrossRefGoogle Scholar
Cowan, DS and Silling, RM (1978) A dynamic, scaled model of accretion at trenches and its implications for the tectonic evolution of subduction complexes. Journal of Geophysical Research–Solid Earth 83, 5389–96.CrossRefGoogle Scholar
Dahlen, FA, Suppe, J and Davis, D (1984) Mechanics of fold-and-thrust belts and accretionary wedges: Cohesive Coulomb Theory. Journal of Geophysical Research – Solid Earth 89, 10087–101, doi:10.1029/JB089iB12p10087.CrossRefGoogle Scholar
DeMets, C, Gordon, RG and Argus, DF (2010) Geologically current plate motion. Geophysical Journal International 181, 1–80.CrossRefGoogle Scholar
Deng, J, Liu, X-F, Wang, Q-F, Dilek, Y and Liang, Y (2017) Isotopic characterization and petrogenetic modeling of Early Cretaceous mafic diking – lithospheric extension in the North China Craton, Eastern Asia. Geological Society of America Bulletin 129, 1379–407, doi:10.1130/B31609.1.CrossRefGoogle Scholar
Dercourt, J, Zonenshain, LP, Ricou, L-E, Kazmin, VG, Le Pichon, X, Knipper, AL, Grandjacquet, C, Sbortshikov, IM, Geyssant, J, Lepvrier, C, Pechersky, DH, Boulin, J, Sibuet, J-C, Savostin, LA, Sorokhtin, O, Westphal, M, Bazhenov, ML, Lauer, JP and Biju-Duval, B (1986) Geological evolution of the Tethys belt from the Atlantic to the Pamirs since the LIAS. Tectonophysics 123, 241–315.10.1016/0040-1951(86)90199-XCrossRefGoogle Scholar
Dickinson, WR (2004) Evolution of the North American Cordillera. Annual Review of Earth and Planetary Sciences 32, 13–45.10.1146/annurev.earth.32.101802.120257CrossRefGoogle Scholar
Dickinson, WR (2008) Accretionary Mesozoic–Cenozoic expansion of the Cordilleran continental margin in California and adjacent Oregon. Geosphere 4, 329–53, doi: 10.1130/GES00105.1.CrossRefGoogle Scholar
Dilek, Y (2003a) Ophiolite concept and its evolution. In Ophiolite Concept and the Evolution of Geological Thought (eds Dilek, Y and Newcomb, S), pp. 1–16. Boulder: Geological Society of America, Special Paper no. 373.CrossRefGoogle Scholar
Dilek, Y (2003 b) Ophiolite pulses, mantle plumes and orogeny. In Ophiolites in Earth History (eds Dilek, Y & Robinson, Paul T), pp. 9–19. Geological Society of London, Special Publication no. 218, doi: 10.1144/GSL.SP.2003.218.01.02.Google Scholar
Dilek, Y (2006) Collision tectonics of the Eastern Mediterranean region: causes and consequences. In Postcollisional Tectonics and Magmatism in the Mediterranean Region and Asia (eds Dilek, Y and Pavlides, S), pp. 1–13. Boulder: Geological Society of America, Special Paper no. 409, doi: 10.1130/2006.2409(1).CrossRefGoogle Scholar
Dilek, Y and Altunkaynak, S (2009) Geochemical and temporal evolution of Cenozoic magmatism in western Turkey: Mantle response to collision, slab breakoff, and lithospheric tearing in an orogenic belt. In Collision and Collapse at the Africa-Arabia-Eurasia Subduction Zone (eds Van Hinsbergen, DJJ, Edwards, MA and Govers, R), pp. 231–33. Geological Society of London, Special Publication no. 311, doi: 10.1144/SP311.8.Google Scholar
Dilek, Y and Altunkaynak, Ş (2010) Geochemistry of Neogene–Quaternary alkaline volcanism in western Anatolia, Turkey, and implications for the Aegean mantle. International Geology Review 52, 631–55, doi: 10.1080/00206810903495020.CrossRefGoogle Scholar
Dilek, Y and Eddy, CA (1992) The Troodos (Cyprus) and Kizildag (S. Turkey) ophiolites as structural models for slow-spreading ridge segments. Journal of Geology 100, 305–22.10.1086/629634CrossRefGoogle Scholar
Dilek, Y and Flower, MFJ (2003) Arc-trench rollback and forearc accretion: 2. A model template for ophiolites in Albania, Cyprus, and Oman. In Ophiolites in Earth History (eds Dilek, Y and Robinson, PT), pp. 43–68. Geological Society of London, Special Publication no. 218.Google Scholar
Dilek, Y and Furnes, H (2009) Structure and geochemistry of Tethyan ophiolites and their petrogenesis in subduction rollback systems. Lithos 13, 1–20, doi: 10.1016/j.lithos.2009.04.022.CrossRefGoogle Scholar
Dilek, Y and Furnes, H (2011) Ophiolite genesis and global tectonics: geochemical and tectonic fingerprinting of ancient oceanic lithosphere. Geological Society of America Bulletin 123, 387–411, doi: 10.1130/B30446.1.CrossRefGoogle Scholar
Dilek, Y and Furnes, Y (2014) Origins of ophiolites. Elements 10, 93–100, doi: 10.2013/gselements.10.2.93.CrossRefGoogle Scholar
Dilek, Y and Furnes, Y (2019) Tethyan ophiolites and Tethyan seaways. Journal of the Geological Society of London 176, 899–912, doi: 10.1144/jgs2019-129.CrossRefGoogle Scholar
Dilek, Y, Furnes, H and Shallo, M (2007) Suprasubduction zone ophiolite formation along the periphery of Mesozoic Gondwana. Gondwana Research 11, 453–475, doi: 10.1016/j.gr.2007.01.005.CrossRefGoogle Scholar
Dilek, Y, Imamverdiyev, N and Altunkaynak, Ş (2010) Geochemistry and tectonics of Cenozoic volcanism in the Lesser Caucasus (Azerbaijan) and the peri-Arabian region: collision-induced mantle dynamics and its magmatic finger-print. International Geology Review 52, 536–78.CrossRefGoogle Scholar
Dilek, Y and Moores, EM (1999) A Tibetan model for the Early Tertiary western United States. Journal of the Geological Society of London 156, 929–42, doi: 10.1144/gsjgs.156.6.0929.CrossRefGoogle Scholar
Dilek, Y and Tang, LM (2020) Magmatic record of the Mesozoic geology of Hainan Island and its implications for the Mesozoic tectonomagmatic evolution of SE China: effects of slab geometry and dynamics in continental tectonics. Geological Magazine, published online ??, doi: https://doi.org/10.1017/S0016756820001211.CrossRefGoogle Scholar
Dilek, Y, Thy, P, Moores, EM and Ramsden, TW (1990) Tectonic evolution of the Troodos ophiolite within the Tethyan framework. Tectonics 9, 811–23, doi: 10.1029/TC009i004p00811.CrossRefGoogle Scholar
Dilek, Y and Whitney, D (2000) Cenozoic crustal evolution in central Anatolia: Extension, magmatism and landscape development: In Proceedings of the Third International Conference on the Geology of the Eastern Mediterranean (eds Panayides, I, Xenophontos, C and Malpas, J), pp. 183–92. Geological Survey Department, September 1998, Nicosia, Cyprus.Google Scholar
Dilek, Y and Yang, J-S (2018) Ophiolites, diamonds, and ultrahigh-pressure minerals: new discoveries and concepts on upper mantle petrogenesis. Lithosphere 10, 3–13, doi: 10.1130/L715.1.CrossRefGoogle Scholar
Doglioni, C, Carminati, E and Cuffaro, M (2006) Simple kinematics of subduction zones. International Geology Review 48, 479–93.CrossRefGoogle Scholar
Doglioni, C, Harabaglia, P, Merlini, S, Mongelli, F, Peccerillo, A and Piromallo, C (1999) Orogens and slabs vs. their direction of subduction. Earth-Science Reviews 45, 167–208.CrossRefGoogle Scholar
Draut, A, Clift, PD, Amato, JM, Blusztajn, J and Schouten, H (2009) Arc-continent collision and the formation of continental crust: a new geochemical and isotopic record from the Ordovician Tyrone Complex, Ireland. Journal of the Geological Society of London 166, 485–500.CrossRefGoogle Scholar
Ducea, MN, Kidder, S, Chesley, JT and Saleeby, JB (2009) Tectonic underplating of trench sediments beneath magmatic arcs: the central California example. International Geology Review 51, doi: 10.1080/00206810802602767.CrossRefGoogle Scholar
Ducea, M, Saleeby, JB and Bergantz, G (2015) The architecture, chemistry, and evolution of continental magmatic arcs. Annual Review of Earth and Planetary Sciences 43, 10.1–10.33, doi: 10.1146/annurev-earth-060614-105049.CrossRefGoogle Scholar
Farris, DW and Haeussler, PJ (2020) Selected geologic maps of the Kodiak batholith and other Paleocene intrusive rocks, Kodiak Island, Alaska. US Geological Survey Scientific Investigations Map 3441, pamphlet 10 p., scale 1:50,000, doi: 10.3133/sim3441.CrossRefGoogle Scholar
Feng, G, Dilek, Y, Niu, X, Liu, F and Yang, J (2018) Geochemistry and geochronology of OIB-type, Early Jurassic magmatism in the Zhangguangcai range, NE China, as a result of continental backarc extension. Geological Magazine, published online 19 November 2018, doi: 10.1017/S0016756818000705.CrossRefGoogle Scholar
Fox, KF, Fleck, RJ, Curtis, GH and Meyer, CE (1985) Implications of the northwestwardly younger age of the volcanic rocks of west-central California. Geological Society of America Bulletin 96, 647–54.2.0.CO;2>CrossRefGoogle Scholar
Furnes, H, Dilek, Y, Zhao, G-C, Safonova, I and Santosh, M (2020) Geochemical characterization of ophiolites in the Alpine-Himalayan orogenic belt: magmatically and tectonically diverse evolution of the Mesozoic Neotethyan oceanic crust. Earth-Science Reviews 208, 103258, doi:10.1016/j.earscirev.2020.103258.CrossRefGoogle Scholar
Geng, Y-S, Shen, QH and Song, H-X (2018) Metamorphic petrology and geology in China: a review. China Geology 1, 137–57.CrossRefGoogle Scholar
Hall, R (2012) Late Jurassic–Cenozoic reconstructions of the Indonesian region and the Indian Ocean. Tectonophysics 570–571, 1–41, doi: 10.1016/j.tecto.2012.04.021.CrossRefGoogle Scholar
Hall, R and Spakman, W (2015) Mantle structure and tectonic history of SE Asia. Tectonophysics 658, 14–45, doi: 10.1016/j.tecto.2015.07.003.CrossRefGoogle Scholar
Hawkesworth, CJ and Kemp, AIS (2006) The differentiation and rates of generation of the continental crust. Chemical Geology 226, 134–43.CrossRefGoogle Scholar
Hibbard, JP and Karig, DE (1990) Structural and magmatic responses to spreading ridge subduction: an example from southwest Japan. Tectonics 9, 207–30.CrossRefGoogle Scholar
Hilde, TWC (1982) Sediment subduction versus accretion around the Pacific. Tectonophysics 99, 381–97.CrossRefGoogle Scholar
Hill, M, Morris, J and Whelan, J (1981) Hybrid granodiorites intruding the accretionary prism, Kodiak, Shumagin, and Sanak Islands, southwest Alaska. Journal of Geophysical Research 86, 10569–90.CrossRefGoogle Scholar
Huang, CY, Yuan, PB and Tsao, SJ (2006) Temporal and spatial records of active arc-continent collision in Taiwan: a synthesis. Geological Society of America Bulletin 118, 274–88, doi: 10.1130/B25527.1.CrossRefGoogle Scholar
Huang, Z, Zhao, D and Wang, L (2015) P wave tomography and anisotropy beneath Southeast Asia: Insight into mantle dynamics. Journal of Geophysical Research, Solid Earth 120, 5154–74, doi: 10.1002/2015JB012098.CrossRefGoogle Scholar
Isozaki, I, Maruyama, S and Furuoka, F (1990) Accreted oceanic materials in Japan. Tectonophysics 181, 179–205.CrossRefGoogle Scholar
Jahn, B-M (2010) Accretionary orogen and evolution of the Japanese Islands: implications from a Sr-Nd isotopic study of the Phanerozoic granitoids from SW Japan. American Journal of Science 310, 1210–49, doi: 10.2475/10.2010.02.CrossRefGoogle Scholar
Jamali, H, Dilek, Y, Daliran, F, Yaghubpur, A and Mehrabi, B (2010) Metallogeny and tectonic evolution of the Cenozoic Ahar-Arasbaran volcanic belt, northern Iran. International Geology Review 52, 608–630, doi: 10.1080/00206810903416323.CrossRefGoogle Scholar
Jarard, RD (1986) Relations among subduction parameters. Reviews in Geophysics 24, 217–84, doi: 10.1029/RG024i002p00217.CrossRefGoogle Scholar
Jolivet, L, Faccenna, C, Goffé, B, Burov, E and Agard, P (2003) Subduction tectonics and exhumation of high-pressure metamorphic rocks in the Mediterranean orogens. American Journal of Science 303, 353–409, doi: 10.2475/ajs.303.5.353.CrossRefGoogle Scholar
Kant, LB, Tepper, JH, Eddy, MP and Nelson, BK (2018) Eocene basalt of Summit Creek: slab breakoff magmatism in the central Washington Cascades, USA. Lithosphere 10, 792–805.Google Scholar
Kawamura, K and Ogawa, Y (2018) Internal structure, active tectonics and dynamic topography of the eastern Nankai accretionary prism toe, Japan, and its tsunamigenic potential. Geological Magazine, published online 30 October 2018, doi: 10.1017/S0016756818000699.CrossRefGoogle Scholar
Kawamura, K, Ogawa, Y, Anma, R, Yokoyama, S, Kawakami, S, Dilek, Y, Moore, GF, Hirano, S, Yamaguchi, A, Sasaki, T and YK05-08 Leg 2 and YK06-02 Shipboard Scientific Parties (2009) Structural architecture and active deformation of the Nankai Accretionary Prism, Japan: submersible survey results from the Tenryu Submarine Canyon. Geological Society of America Bulletin 121, 1629–46.CrossRefGoogle Scholar
Kawamura, K, Sasaki, T, Kanamatsu, T, Sakaguchi, A and Ogawa, Y (2012) Large submarine landslides in the Japan Trench: a new scenario for additional tsunami generation. Geophysical Research Letters 39, L05308.CrossRefGoogle Scholar
Kay, SM, Godoy, E and Andrew, K (2005) Episodic arc migration, crustal thickening, subduction erosion, and magmatism in the south-central Andes. Geological Society of America Bulletin 117, 67–88, doi: 10.1130/B25431.1.CrossRefGoogle Scholar
Kimura, G, Koge, H and Tsuji, T (2018) Punctuated growth of an accretionary prism and the onset of a seismogenic megathrust in the Nankai Trough. Progress in Earth and Planetary Science 5, 78, doi:10.1186/s40645-018-0234-1.CrossRefGoogle Scholar
Kimura, J-I and Yoshida, T (2006) Contributions of slab fluid, mantle wedge and crust to the origin of Quaternary lavas in the NE Japan arc. Journal of Petrology 47, 2185–232.CrossRefGoogle Scholar
Langenheim, VE, Jachens, RC, Wentworth, CM and McLaughlin, RJ (2013) Previously unrecognized regional structure of the Coastal Belt of the Franciscan Complex, northern California, revealed by magnetic data. Geosphere 9, 1514–29, doi: 10.1130/GES00942.1.CrossRefGoogle Scholar
Le Pichon, X, Wmant, S, Tokuyama, H, Thoué, F, Huchon, P and Henry, P (1996) Structure and evolution of the backstop in the eastern Nankai Trough area (Japan): implications for the soon-to-come Tokai earthquake. Island Arc 5, 440–54, doi: 10.1111/j.1440-1738.1996.tb00164.x.CrossRefGoogle Scholar
Li, JH, Dong, S, Cawood, PA, Zhao, G, Johnson, ST, Zhang, Y and Xin, Y (2018) An Andean-type retro-arc foreland system beneath northwest South China revealed by SINOPROBE profiling. Earth and Planetary Science Letters 490, 170–79.CrossRefGoogle Scholar
Li, J, Shillington, DJ, Bécel, A, Nedimović, MR, Webb, SC, Saffer, DM, Keranen, KM and Kuehn, H (2015a) Downdip variations in seismic reflection character: implications for fault structure and seismogenic behavior in the Alaska subduction zone. Journal of Geophysical Research – Solid Earth 120, doi: 10.1002/2015JB012338.CrossRefGoogle Scholar
Li, Y, Yang, J-S, Dilek, Y, Zhang, J, Pei, X, Chen, S-Y, Xu, X-Z and Li, J (2015b) Crustal architecture of the Shangdan suture zone in the early Paleozoic Qinling orogenic belt, China: record of subduction initiation and backarc basin development. Gondwana Research 27, 733–44, doi: 10.1016/j.gr.2014.03.006.CrossRefGoogle Scholar
Li, ZX and Li, XH (2007) Formation of the 1300-km-wide intracontinental orogen and post orogenic magmatic province in Mesozoic South China: a flat-slab subduction model. Geology 35, 179–82.CrossRefGoogle Scholar
Lister, G and Foster, M (2009) Tectonic mode switches and the nature of orogenesis. Lithos 113, 274–91.CrossRefGoogle Scholar
Liu, F, Dilek, Y, Xie, Y-X, Yang, J-S and Lian, D-Y (2018) Melt evolution of upper mantle peridotites and mafic dikes in the northern ophiolite belt of the western Yarlung Zangbo suture zone (southern Tibet). Lithosphere 10, 109–32, doi: 10.1130/L689.1.CrossRefGoogle Scholar
Llytwyn, J, Gilbert, S, Casey, J and Kusky, TM (2000) Geochemistry of near-trench intrusives associated with ridge subduction, Seldovia quadrangle, southern Alaska. Journal of Geophysical Research 105, 27957–78.CrossRefGoogle Scholar
MacPherson, GJ, Phipps, SP and Grossman, JN (1990) Diverse sources for igneous blocks in Franciscan melanges, California Coast Ranges. Journal of Geology 98, 845–62.CrossRefGoogle Scholar
Malavieille, J, Dominguez, S, Lu, C-Y, Chen, C-T and Konstantinovskaya, E (2019) Deformation partitioning in mountain belts: insights from analogue modelling experiments and the Taiwan collisional orogen. Geological Magazine, published online 11 July 2019, doi: 10.1017/S0016756819000645.CrossRefGoogle Scholar
Mann, P (2007) Overview of the tectonic history of northern Central America. In Geologic and Tectonic Development of the Caribbean Plate Boundary in Northern Central America (ed. Mann, P), pp. 1–19. Boulder: Geological Society of America, Special Paper no. 428.CrossRefGoogle Scholar
Mao, Q, Xiao, W, Windley, BF, Yu, M, Sun, M, Ao, S and Zhang, J (2019) Early Permian subduction-related transtension in the Turpan Basin, East Tianshan (NW China): implications for accretionary tectonics of the southern Altaids. Geological Magazine, published online 14 November 2019, doi: 10.1017/S0016756819001006.CrossRefGoogle Scholar
Maruyama, S, Isozaki, Y, Kimura, G and Terabayashi, M (1997) Paleogeographic maps of the Japanese Islands: plate tectonic synthesis from 750Ma to the present. Island Arc 6, 121–42.CrossRefGoogle Scholar
Masson, DG, Harbitz, CB, Wynn, RB, Pedersen, G and Lovholt, F (2006) Submarine landslides: processes, triggers and hazard prediction. Philosophical Transactions of the Royal Society A364, 2009–39.Google Scholar
Meneghini, F, Marroni, M, Moore, JC, Pandolfi, L and Rowe, CD (2009) The processes of underthrusting and underplating in the geologic record: structural diversity between the Franciscan Complex (California), the Kodiak Complex (Alaska) and the Internal Ligurian Units (Italy). Geological Journal 44(2), 126–52, doi: 10.1002/gj.1144.CrossRefGoogle Scholar
Metcalfe, I (1994) Gondwana origin, dispersion, and accretion of East and Southeast Asian continental terranes. Journal of South American Earth Sciences 7, 333–47, doi: 10.1016/0895-9811(94)90019-1.CrossRefGoogle Scholar
Monger, JWH and Francheteau, J (Editors) (1987) Circum-Pacific Orogenic Belts and Evolution of the Pacific Ocean Basin. Washington: American Geophysical Union, Geodynamics Series no. 18, doi: 10.1029/GD018.CrossRefGoogle Scholar
Moore, GF, Park, JO, Bangs, NL, Gulick, SP, Tobin, HJ, Nakamura, Y, Sato, S, Tsuji, T, Yoro, T, Tanaka, H, Urakki, S, Kido, Y, Sanada, Y Kuramoto, S and Taira, A (2009) Structural and seismic stratigraphic framework of the NanTroSEIZE stage 1 transect. In Proceedings of the Integrated Ocean Drilling Program. Washington: IODP, volume 314/315/316, doi: 10.2204/iodp.proc.314315316.102.2009.CrossRefGoogle Scholar
Moore, JC, Biju-Duval, B, Bergen, JA, Blackington, G, Claypool, GE, Cowan, DS, Duennebier, F, Guerra, RT, Hemleben, CH, Hussong, D, Marlow, MS, Natland, JH, Pudsey, CJ, Renz, GW, Tardy, M, Willis, ME, Wilson, D and Wright, AA (1982) Offscraping and underthrusting of sediment at the deformation front of the Barbados Ridge: Deep Sea Drilling Project Leg 78A. Geological Society of America Bulletin 93, 1065–77.2.0.CO;2>CrossRefGoogle Scholar
Moores, EM and Twiss, RJ (1995) Tectonics. New York: WH Freeman & Company, 415 pp.Google Scholar
Nishiyama, T, Ohfuji, H, Fukuba, K, Terauchi, M, Nishi, U, Harada, K, Unoki, K, Moribe, Y, Yoshiasa, A, Ishimaru, S, Mori, Y, Shigeno, M and Arai, S (2020) Microdiamond in a low-grade metapelite from a Cretaceous subduction complex, western Kyushu, Japan. Nature Scientific Reports 10, 11645, doi: 10.1038/s41598-020-68599-7.CrossRefGoogle Scholar
Nitta, S, Kasaya, T and Kawamura, K (2018) Active sediment creep deformation on a deep-sea terrace in the Japan Trench. Geological Magazine, published online 28 December 2018, doi: 10.1017/S0016756818000894.CrossRefGoogle Scholar
Niu, X-L, Dilek, Y, Liu, F, Feng, G and Yang, J (2019) Early Devonian ultrapotassic magmatism in the North China Craton: geochemical and isotopic evidence for subcontinental lithospheric mantle metasomatism by subducted sediment-derived fluids. Geological Magazine, published online 6 August 2019, doi: 10.1017/S0016756819000797.CrossRefGoogle Scholar
Niu, X-L, Liu, F, Yang, J-S, Dilek, Y, Xu, Z-Q, Feng, G, Xiong, F, Tian, Y and Sein, K (2018) Mineralogy and petrology of the Kalaymyo peridotite massif, Indo-Myanmar Ranges, western Myanmar. Lithosphere 10, 79–94, doi: 10.1130/L589.1.Google Scholar
Noda, A, Koge, H, Yamada, Y, Miyakawa, A and Ashi, J (2020) Subduction of trench-fill sediments beneath an accretionary wedge: insights from sandbox analogue experiments. Geosphere 16, 953–68.CrossRefGoogle Scholar
Ogawa, Y, Mori, R, Tsunogae, T, Dilek, Y and Harris, R (2014) New interpretation of the Franciscan mélange at San Simeon coast, California: tectonic intrusion into an accretionary prism. International Geology Review 57(5–8), 824–42, doi: 10.1080/00206814.2014.968813.CrossRefGoogle Scholar
Onishi, CT, Kimura, G, Hashimoto, Y, Ikehara-Ohmori, K and Watanabe, T (2001) Deformation history of tectonic mélange and its relationship to the underplating process and relative plate motion: an example from the deeply buried Shimanto Belt, SW Japan. Tectonics 20, 376–93.CrossRefGoogle Scholar
Park, J-O, Moore, GF, Tsuru, T, Kodaira, S and Kaneda, Y (2004) Subducted oceanic ridge influencing the Nankai megathrust earthquake rupture. Earth and Planetary Science Letters 217, 77–84.CrossRefGoogle Scholar
Park, JO, Tsuru, T, Takahashi, N, Hori, T, Kodaira, S, Nakanishi, A, Miura, S and Kaneda, Y (2002) A deep strong reflector in the Nankai accretionary wedge from multichannel seismic data: Implications for underplating and interseismic shear stress release. Journal of Geophysical Research 107, ESE 3-16, doi:10.1029/2001JB000262.CrossRefGoogle Scholar
Pérez-Flores, P, Cembrano, J, Sánchez-Alfaro, P, Veloso, E, Arancibia, G and Roquer, T (2016) Tectonics, magmatism and paleo-fluid distribution in a strike-slip setting: insights from the northern termination of the Liquine–Ofqui fault System, Chile. Tectonophysics 680, 192–210.CrossRefGoogle Scholar
Plank, T (2005) Constraints from Thorium/Lanthanum on sediment recycling at subduction zones and the evolution of the continents. Journal of Petrology 46, 921–44.CrossRefGoogle Scholar
Platt, JP (1986) Dynamics of orogenic wedges, and the uplift of high-pressure metamorphic rocks. Geological Society of America Bulletin 97, 1106–21.2.0.CO;2>CrossRefGoogle Scholar
Rehman, HU (2018) Geochronological enigma of the high- and ultrahigh-pressure rocks in the Himalayan orogen. In HP–UHP Metamorphism and Tectonic Evolution of Orogenic Belts (eds Zhang, LF, Zhang, Z, Schertl, H-P and Wei, C) Geological Society of London, Special Publication no. 474, doi: 10.1144/SP474.14.Google Scholar
Replumaz, A, Karason, H, van der Hilst, RD, Besse, J and Tapponnier, P (2004) 4-D evolution of SE Asia’s mantle from geological reconstructions and seismic tomography. Earth and Planetary Science Letters 221, 103–15, doi: 10.1016/S0012-821X(04)00070-6.CrossRefGoogle Scholar
Safonova, I, Maruyama, S, Kruk, N, Obut, O, Kotler, P, Gavryushkina, O, Khromykh, S, Kuibida, M and Krivonogov, S (2018) Pacific-type orogenic belts: linking evolution of oceans, active margins and intra-plate magmatism. Episodes 41, 79–98, doi: 10.18814/epiiugs/2018/018008.CrossRefGoogle Scholar
Sakai, S, Hirano, N, Dilek, Y, Machida, S, Yasukawa, K and Kato, Y (2019) Tokoro Belt (NE Hokkaido): an exhumed, Jurassic – Early Cretaceous seamount in the Late Cretaceous accretionary prism of northern Japan. Geological Magazine, published online 24 June 2019, doi: 10.1017/S0016756819000633.CrossRefGoogle Scholar
Sarıfakıoğlu, E, Dilek, Y and Sevin, M (2017) New synthesis of the Izmir-Ankara-Erzincan suture zone and the Ankara mélange in northern Anatolia based on new geochemical and geochronological constraints. In Tectonic Evolution, Collision, and Seismicity of Southwest Asia: In Honor of Manuel Berberian’s Forty-Five Years of Research Contributions (ed. Sorkhabi, R), pp. 613–75. Washington: Geological Society of America, Special Paper no. 525, doi: 10.1130/2017.2525(19).Google Scholar
Sato, K, Vrublevsky, AA, Rodionov, SM, Pomanovsky, NP and Nedachi, M (2002) Mid-Cretaceous episodic magmatism and tin mineralization in Khingan–Okhotsk volcan-plutonic belt, Far East Russia. Resource Geology 52, 1–14.CrossRefGoogle Scholar
Schellart, WP (2020) Control of subduction zone age and size on flat slab subduction. Frontiers in Earth Science 8, 26, doi: 10.3389/feart.2020.00026.CrossRefGoogle Scholar
Schellart, WP, Freeman, J, Stegman, DR, Moresi, L and May, D (2007) Evolution and diversity of subduction zones controlled by slab width. Nature 446, 308–11, doi: 10.1038/nature05615.CrossRefGoogle ScholarPubMed
Schellart, WP and Rawlinson, N (2013) Global correlations between maximum magnitudes of subduction zone interface thrust earthquakes and physical parameters of subduction zones. Physics of the Earth and Planetary Interiors 225, 41–67.CrossRefGoogle Scholar
Scholl, DW (2019) Seismic imaging evidence that forearc underplating built the accretionary rock record of coastal North and South America. Geological Magazine, published online 9 September 2019, doi: 10.1017/S0016756819000955.CrossRefGoogle Scholar
Scholl, DW and von Huene, R (2009) Implications of estimated magmatic additions and recycling losses at the subduction zones of accretionary (non-collisional) and collisional (suturing) orogens. In Accretionary Orogens in Space and Time (eds Cawood, P and Kröner, A), pp. 105–25. Geological Society of London, Special Publication no. 318.Google Scholar
Screaton, EJ, Kimura, G, Curewitz, D, Moore, G, Chester, F, Fabbri, O, Fergusson, C, Girault, F, Goldsby, D, Harris, R, Inagaki, F, Jiang, T, Kitamura, Y, Knuth, M, Li, CF, Liljedahl, LC, Louis, L, Milliken, K, Nicholson, U, Riedinger, N, Sakaguchi, A, Solomon, E, Strasser, M, Su, X, Tsutsumi, A, Yamaguchi, A, Ujie, K and Zhao, X (2009) Interactions between deformation and fluids in the frontal thrust region of the NanTroSEIZE transect offshore the Kii Peninsula, Japan: results from IODP Expedition 316 Sites C0006 and C0007. Geochemistry, Geophysics, Geosystems 10(12), doi:10.1029/2009GC002713.CrossRefGoogle Scholar
Shillington, DJ, Van Avendonk, HJA, Holbrook, WS, Kelemen, PB and Hornbach, MJ (2004) Composition and structure of the central Aleutian island arc from arc-parallel wide-angle seismic data. Geochemistry, Geophysics, Geosystems 5, Q10006, doi: 10.1029/2004GC000715.CrossRefGoogle Scholar
Shinjoe, H, Orihashi, Y and Anma, R (2019) U–Pb ages of Miocene near-trench granitic rocks of the Southwest Japan arc: implications for magmatism related to hot subduction. Geological Magazine, published online 7 November 2019, doi: 10.1017/S0016756819000785.CrossRefGoogle Scholar
Shreve, RL and Cloos, M (1986) Dynamics of sediment subduction, melange formation, and prism accretion. Journal of Geophysical Research–Solid Earth 91, 10229–45, doi:10.1029/JB091iB10p10229.CrossRefGoogle Scholar
Sieh, K and Natawidjaja, D (2000) Neotectonics of the Sumatran Fault, Indonesia. Journal of Geophysical Research–Solid Earth 105, 28295–326.CrossRefGoogle Scholar
Sisson, VB, Pavlis, TL, Roeske, SM and Thorkelson, DJ (2003) Introduction: An overview of ridge-trench interactions in modern and ancient settings. In Geology of a Transpressional Orogen Developed During Ridge-Trench Interaction along the North Pacific Margin (eds Sisson, VB, Roeske, SM and Pavlis, TL), pp. 1–18. Washington: Geological Society of America, Special Paper no. 371.CrossRefGoogle Scholar
Stampfli, GM (2000) Tethyan oceans. In Tectonics and Magmatism in Turkey and the Surrounding Area (eds Bozkurt, E, Winchester, JA and Piper, JDA), pp. 1–23. Geological Society of London, Special Publication no. 173.Google Scholar
Stern, CR (2011) Subduction erosion: rates, mechanisms, and its role in arc magmatism and the evolution of the continental crust and mantle. Gondwana Research 20(2–3), 284–308, doi: 10.1016/j.gr.2011.03.006.CrossRefGoogle Scholar
Suppe, J (1981) Mechanics of mountain-building and metamorphism in Taiwan. Memoir of the Geological Society of China 4, 67–89.Google Scholar
Taira, A (2001) Tectonic evolution of the Japanese island arc system. Annual Review of Earth & Planetary Sciences 29, 109–34.CrossRefGoogle Scholar
Takahashi, N, Kodaira, S, Tatsumi, Y, Kaneda, Y and Suyehiro, K (2008) Structure and growth of the Izu-Bonin-Mariana arc crust: 1. Seismic constraint on crust and mantle structure of the Mariana arc–back-arc system. Journal of Geophysical Research 113, B1, doi: 10.1029/2007JB005120.CrossRefGoogle Scholar
Tankut, A, Dilek, Y and Onen, P (1998) Petrology and geochemistry of the Neo-Tethyan volcanism as revealed in the Ankara Mélange, Turkey. Journal of Volcanological & Geothermal Research 85, 265–84.CrossRefGoogle Scholar
Tappin, DR, Grilli, ST, Harris, JC, Geller, RJ, Masterlark, T, Kirby, JT, Shi, F, Ma, G, Thingbaijam, KKS and Mai, PM (2014) Did a submarine landslide contribute to the 2011 Tohoku tsunami? Marine Geology 357, 344–61.CrossRefGoogle Scholar
Tatsumi, Y, Shukuno, H, Tani, K, Takahashi, N, Kodaira, S and Kogiso, T (2008) Structure and growth of the Izu-Bonin-Mariana arc crust: 2. Role of crust-mantle transformation and the transparent Moho in arc crust evolution. Journal of Geophysical Research 113, B02203, doi: 10.1029/2007JB005121.CrossRefGoogle Scholar
Terabayashi, M, Okamato, K, Yamamato, H, Kaneko, Y, Maruyama, S, Katayama, I, Tsutomu, O, Komiya, T, Ishikawa, A, Anma, R, Ozawa, H, Windley, BF and Liou, JG (2005) Accretionary complex Origin of the mafic-ultramafic bodies of the Sanbagawa Belt, Central Shikoku, Japan. International Geology Review 47, 1058–73.CrossRefGoogle Scholar
Thorkelson, DJ and Taylor, RP (1989) Cordilleran slab windows. Geology 17, 833–36.2.3.CO;2>CrossRefGoogle Scholar
Tian, Z-X, Yan, Y, Huang, C-Y, Dilek, Y, Yu, M-M, Liu, H-Q, Zhang, X-C and Zhang, Y (2020) Fingerprinting Subducted Oceanic Crust and Hainan Plume in the Melt Sources of Cenozoic Basalts from the South China Sea Region. Terra Nova, published online 8 July 2020, doi: 10.1111/TER.12486.CrossRefGoogle Scholar
Underwood, MB (2018) The origin of strata within the inner accretionary prism of Nankai Trough: evidence from clay mineral assemblages along the NanTroSEIZE transect. Island Arc 27, e12252.CrossRefGoogle Scholar
Underwood, MB, Byrne, T, Hibbard, JP, DiTullio, L and Laughland, MM (1993) The effects of ridge subduction on the thermal structure of accretionary prisms: a Tertiary example from the Shimanto Belt of Japan. Geological Society of America Special Paper 273, doi: 10.1130/SPE273.CrossRefGoogle Scholar
von Huene, R, Miller, JJ and Krabbenhoeft, A (2019) The Shumagin seismic gap structure and associated tsunami hazards, Alaska convergent margin. Geosphere 15, 324–41, doi: 10.1130/GES01657.1.CrossRefGoogle Scholar
von Huene, R, Ranero, CR and Vannucchi, P (2004) Generic model of subduction erosion. Geology 32, 913–16.CrossRefGoogle Scholar
von Huene, R and Scholl, DW (1991) Observations at convergent margins concerning sediment subduction, subduction erosion, and the growth of continental crust. Reviews of Geophysics 29, 279–316.CrossRefGoogle Scholar
Wakita, K, Nakagawa, T, Sakata, M, Tanaka, N and Oyama, N (2018) Phanerozoic accretionary history of Japan and the western Pacific margin. Geological Magazine, published online 18 December 2018, doi: 10.1017/S0016756818000742.CrossRefGoogle Scholar
Watkins, JS, Moore, JC, Shipley, TH, Bachman, SB, Beghtet, FW, Butt, A, Oidyk, BM, Leggett, JK, Lundberg, N, McMillen, KJ, Niitsuma, N, Shepherd, LE, Stephan, JF and Stradner, H (1981) Accretion, underplating, subduction and tectonic evolution, Middle America Trench, Southern Mexico: results from DSDP Leg 66. Oceanologica Acta, Special Issue, 213–24, Open access: https://archimer.ifremer.fr/doc/00245/35668/.Google Scholar
Wilhem, C, Windley, B and Stampfli, G (2012) The Altaids of Central Asia: a tectonic and evolutionary innovative review. Earth-Science Reviews 113, 303–41, doi: 10.1016/j.earscirev.2012.04.001.CrossRefGoogle Scholar
Wu, F-Y, Yang, J-H, Xu, Y-G, Wilde, SA and Walker, RJ (2019) Destruction of the north China Craton in the Mesozoic. Annual Review of Earth and Planetary Sciences 47, 173–95, doi: 10.1146/annurev-earth-053018-060342.CrossRefGoogle Scholar
Xiao, WJ, Windley, BF, Hao, J and Zhai, MG (2003) Accretion leading to collision and the Permian Solonker suture, Inner Mongolia, China: termination of the central Asian orogenic belt. Tectonics 22, published online 4 December 2003, doi: 10.1029/2002TC001484.CrossRefGoogle Scholar
Xu, Z-Q, Dilek, Y, Yang, J-S, Liang, F-H, Liu, F, Ba, D-Z, Cai, Z-H, Li, G-W, Dong, H-W and Ji, SC (2015) Crustal structure of the Indus–Tsangpo suture zone and its ophiolites in southern Tibet. Gondwana Research 27, 507–24, doi: 10.1016/j.gr.2014.08.001.CrossRefGoogle Scholar
Yu, M-M, Dilek, Y, Yumul, GP Jr, Yan, Y, Dimalanta, CB and Huang, C-Y (2020) Slab-controlled elemental-isotopic enrichments during subduction initiation magmatism and variations in forearc chemostratigraphy. Earth and Planetary Science Letters 538, 116217, doi:10.1016/j.epsl.2020.116217.CrossRefGoogle Scholar
Zahirovic, S, Seton, M and Múller, RD (2014) The Cretaceous and Cenozoic tectonic evolution of Southeast Asia. Solid Earth 5, 227–73, doi: 10.5194/se-5-227-2014.CrossRefGoogle Scholar
Zhang, F-Q, Chen, H-L, Dilek, Y, Yang, S-F, Meng, Q-A (2017) Late Cretaceous tectonic evolution along NE Asian continental margin: new constraints from the sedimentary and structural records of Cretaceous basin in NE China. Earth Science Reviews 171, 598–620, doi: 10.1016/j.earscirev.2017.05.015.CrossRefGoogle Scholar
Zhang, F-Q, Wu, H-X, Dilek, Y, Zhang, W, Zhu, K-Y and Chen, HL (2019a) Guadalupian (Permian) onset of subduction zone volcanism and geodynamic turnover from passive to active margin tectonics in Southeast China. Geological Society of America Bulletin 132, 130–48, doi: 10.1130/B32014.1.CrossRefGoogle Scholar
Zhang, Y, Dilek, Y, Zhang, F-Q, Chen, H-L and Zhu, C-T (2019b) Seismic structure and tectonics of the Zhanhua Depression in NE China associated with Paleogene slip history and fault kinematics along the Tan-Lu Fault Zone. Tectonophysics 775, published online December 2019, doi: 10.1016/j.tecto.2019.228303.Google Scholar