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Diagenetic and Paleoenvironmental Controls on Late Cretaceous Clay Minerals in the Songliao Basin, Northeast China

Published online by Cambridge University Press:  01 January 2024

Yuan Gao ,
Chengshan Wang ,
Zhifei Liu ,
Xiaojing Du  and
Daniel E. Ibarra
Yuan Gao
Affiliation:
State Key Laboratory of Biogeology and Environmental Geology, School of Earth Sciences and Resources, China University of Geosciences (Beijing), Beijing 100083, China
Chengshan Wang*
Affiliation:
State Key Laboratory of Biogeology and Environmental Geology, School of Earth Sciences and Resources, China University of Geosciences (Beijing), Beijing 100083, China
Zhifei Liu
Affiliation:
State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China
Xiaojing Du
Affiliation:
Department of Earth and Environmental Sciences, University of Michigan, Ann Arbor, Michigan 48109, USA
Daniel E. Ibarra
Affiliation:
Department of Earth System Science, Stanford University, Stanford, California 94305-4216, USA
*
*E-mail address of corresponding author: [email protected]
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Abstract

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Sedimentary and diagenetic processes control the distribution of clay minerals in sedimentary basins, although these processes have seldom been studied continuously in continental sedimentary basins. The Songliao Basin, northeast China, is a large continental, petroleum-bearing basin, and provides a unique study site to understand the sedimentary and diagenetic processes that influence clay assemblages. In this paper, the clay mineralogy of a 2500 m-thick Late Cretaceous (late Turonian to Maastrichtian) terrestrial sedimentary succession (SK-1s and SK-1n cores), retrieved by the International Continental Scientific Drilling Program in the Songliao Basin, was examined. The objective was to determine the diagenetic and paleoenvironmental variations that controlled the formation of clay mineral assemblages, and to determine the thermal and paleoenvironmental evolution of the basin. The results from both cores show that illite is ubiquitous through the succession, smectite is frequently encountered in the upper strata, and ordered mixed-layer illite-smectite (I-S), chlorite, and kaolinite are abundant in the lower strata. Burial diagenesis is the primary control on the observed decrease of smectite and increasing illite, I-S, and chlorite with depth. Observations of clay-mineral diagenesis are used to reconstruct the paleotemperatures and maximum burial depths to which the sediments were subjected. The lowermost sediments could have reached a maximum burial of ~1000 m deeper than today and temperatures ~50°C higher than today in the latest Cretaceous. The transition of smectite to I-S in the SK-1 cores and the inferred paleotemperatures provide new constraints for basin modeling of oil maturation at elevated temperatures in the Songliao Basin. Authigenic kaolinite and smectite are enriched in sandstones with respect to the coeval mudstones from the SK-1n core, as a result of early diagenesis with the participation of primary aluminosilicates and pore fluids. In the upper part of both SK-1 cores, variations in smectite and illite were controlled primarily by paleoenvironmental changes. Increases in smectite and decreases in illite from the late Campanian to Maastrichtian are interpreted as resulting from increasing humidity, a conclusion consistent with previous paleoenvironmental interpretations.

Keywords

Clay MineralsDiagenesisThermal EvolutionPaleoenvironmentLate CretaceousSongliao BasinChina
Type
Article
Information
Clays and Clay Minerals , Volume 63 , Issue 6 , December 2015 , pp. 469 - 484
Copyright
Copyright © The Clay Minerals Society 2015

References

Bjørlykke, K., 1998 Clay mineral diagenesis in sedimentary basins — a key to the prediction of rock properties. Examples from the North Sea Basin Clay Minerals 33 15–34.CrossRefGoogle Scholar
Bjørlykke, K., 2014 Relationships between depositional environments, burial history and rock properties. Some principal aspects of diagenetic process in sedimentary basins Sedimentary Geology 301 1–14.CrossRefGoogle Scholar
Chamberlain, C.P. Wan, X. Graham, S.A. Carroll, A.R. Doebbert, A.C. Sageman, B.B. Blisniuk, P. Kent-Corson, M.L. Wang, Z. and Wang, C., 2013 Stable isotopic evidence for climate and basin evolution of the Late Cretaceous Songliao Basin, China. Palaeogeography, Palaeoclimatology Palaeoecology 385 106–124.CrossRefGoogle Scholar
Chamley, H., 1989 Clay Sedimentology Berlin Springer Verlag 623.CrossRefGoogle Scholar
Chen, P. and Chang, Z., 1994 Nonmarine Cretaceous stratigraphy of eastern China Cretaceous Research 15 245–257.CrossRefGoogle Scholar
Chen, X. Li, Z.Q. Chen, J.L. Li, H.K. and Zhang, T., 2010 Determination of the reverse period of Songliao Basin, China Geological Bulletin of China 29 2/3 305–311.Google Scholar
Cheng, R. Wang, G. Wang, P. and Gao, Y., 2009 Uppermost Cretaceous sediments: sedimentary microfacies and sedimentary environment evolution of Sifangtai Formation and Mingshui Formation in SK-1(n) Earth Science Frontiers 16 6 85–95.Google Scholar
Cuadros, J. Caballero, E. Huertas, F.J. Cisneros, C.J.d. Huertas, F. and Linares, J., 1999 Experimental alteration of volcanic tuff: Smectite formation and effect on 18O isotope composition Clays and Clay Minerals 47 769–776.CrossRefGoogle Scholar
Day-Stirrat, R.J. Milliken, K.L. Dutton, S.P. Loucks, R.G. Hillier, S. Aplin, A.C. and Schleicher, A.M., 2010 Opensystem chemical behavior in deep Wilcox Group mudstones, Texas Gulf Coast, USA Marine and Petroleum Geology 27 1804–1818.CrossRefGoogle Scholar
Deconinck, J.F. Blanc-Valleron, M.M. Rouchy, J.M. Camoin, G. and Badaut-Trauth, D., 2000 Palaeoenvironmental and diagenetic control of the mineralogy of Upper Cretaceous—Lower Tertiary deposits of the Central Palaeo—Andean basin of Bolivia (Potosi area) Sedimentary Geology 132 263–278.CrossRefGoogle Scholar
Deconinck, J.-F. Amédro, F. Baudin, F. Godet, A. Pellenard, P. Robaszynski, F. and Zimmerlin, I., 2005 Late Cretaceous palaeoenvironments expressed by the clay mineralogy of Cenomanian—Campanian chalks from the east of the Paris Basin Cretaceous Research 26 171–179.CrossRefGoogle Scholar
Deconinck, J.F. Crasquin, S. Bruneau, L. Pellenard, P. Baudin, F. and Feng, Q., 2014 Diagenesis of clay minerals and K-bentonites in late Permian/Early Triassic sediments of the Sichuan Basin (Chaotian section, Central China) Journal of Asian Earth Sciences 81 28–37.CrossRefGoogle Scholar
Deng, C.L. He, H.Y. Pan, Y.X. and Zhu, R.X., 2013 Chronology of the terrestrial Upper Cretaceous in the Songliao Basin, northeast Asia Palaeogeography, Palaeoclimatology, Palaeoecology 385 44–54.CrossRefGoogle Scholar
Dera, G. Pellenard, P. Neige, P. Deconinck, J.-F. Pucéat, E. and Dommergues, J.-L., 2009 Distribution of clay minerals in Early Jurassic Peritethyan seas: Palaeoclimatic significance inferred from multiproxy comparisons Palaeogeography, Palaeoclimatology, Palaeoecology 271 39–51.CrossRefGoogle Scholar
Do Campo, M. Nieto, F. del Papa, C. and Hongn, F., 2014 Syn- and post-sedimentary controls on clay mineral assemblages in a tectonically active basin, Andean Argentinean foreland Journal of South American Earth Sciences 52 43–56.CrossRefGoogle Scholar
Elliott, W.C. and Matisoff, G., 1996 Evaluation of kinetic models for the smectite to illite transformation Clays and Clay Minerals 44 77–87.CrossRefGoogle Scholar
Fesharaki, O. García-Romero, E. Cuevas-González, J. and López-Martínez, N., 2007 Clay mineral genesis and chemical evolution in the Miocene sediments of Somosaguas, Madrid Basin, Spain Clay Minerals 42 187–201.CrossRefGoogle Scholar
Feng, Z.Q. Jia, C.Z. Xie, X.N. Zhang, S. Feng, Z.H. and Cross, T.A., 2010 Tectonostratigraphic units and stratigraphic sequences of the nonmarine Songliao Basin, northeast China Basin Research 22 79–95.Google Scholar
Feng, Z. Wang, C. Graham, S. Koeberl, C. Dong, H. Huang, Y. and Gao, Y., 2013 Continental scientific drilling project of Cretaceous Songliao Basin: Scientific objectives and drilling technology Palaeogeography, Palaeoclimatology, Palaeoecology 385 6–16.CrossRefGoogle Scholar
Franke, D. and Ehrmann, W., 2010 Neogene clay mineral assemblages in the AND-2A drill core (McMurdo Sound, Antarctica) and their implications for environmental change Palaeogeography, Palaeoclimatology, Palaeoecology 286 55–65.CrossRefGoogle Scholar
Fu, M. Zhang, S. Ding, X. Liao, Q. Xiong, D. and Zhu, Z., 2012 Characteristics and petroleum geologic significances of clay rims in sandstones of Mingshui Formation, well Songke 1, Songliao Basin Petroleum Geology and Experiment 34 587–592.Google Scholar
Gao, R.Q. Zhao, C.B. Qiao, X.Y. Zheng, Y.L. Yan, F.Y. and Wan, C.B., 1999 Cretaceous Oil Strata Palynology from Songliao Basin Beijing (in Chinese) Geological Publishing House.Google Scholar
Gao, Y. Wang, C. Liu, Z. Zhao, B. and Zhang, X., 2013 Clay mineralogy of the middle Mingshui Formation (upper Campanian to lower Maastrichtian) from the SK-1n borehole in the Songliao Basin, NE China: Implications for palaeoclimate and provenance Palaeogeography, Palaeoclimatology, Palaeoecology 385 162–170.CrossRefGoogle Scholar
Gao, Y. Ibarra, D.E. Wang, C. Caves, J.K. Chamberlain, C.P. Graham, S.A. and Wu, H., 2015 Mid-latitude terrestrial climate of East Asia linked to global climate in the Late Cretaceous Geology 43 287–290.CrossRefGoogle Scholar
Graham, S.A. Hendrix, M.S. Johnson, C.L. Badamgarav, D. Badarch, G. Amory, J. Porter, M. Barsbold, R. Webb, L.E. and Hacker, B.R., 2001 Sedimentary record and tectonic implications of Mesozoic rifting in southeast Mongolia Geological Society of America Bulletin 113 1560–1579.2.0.CO;2>CrossRefGoogle Scholar
Guo, W. Yu, W. Liu, Z. and Ma, L., 2009 The burial history of the southern Songliao Basin Journal of Jilin University (Earth Science Edition) 39 353–360.Google Scholar
He, H. Deng, C. Wang, P. Pan, Y. and Zhu, R., 2012 Toward age determination of the termination of the Cretaceous Normal Superchron Geochemistry, Geophysics, Geosystems 13 Q02002.CrossRefGoogle Scholar
Hong, H. Li, Z. Xue, H. Zhu, Y. Zhang, K. and Xiang, S., 2007 Oligocene clay mineralogy of the Linxia Basin: Evidence of paleoclimatic evolution subsequent to the initial-stage uplift of the Tibetan Plateau Clays and Clay Minerals 55 491–503.CrossRefGoogle Scholar
Hou, Q.J. Feng, Z.Q. and Feng, Z.H., 2009 Terrestrial Petroleum Geology of Songliao Basin Beijing (in Chinese) Petroleum Industry Press.Google Scholar
Hower, J. Eslinger, E.V. Hower, M.E. and Perry, E.A., 1976 Mechanism of burial metamorphism of argillaceous sediment: 1. Mineralogical and chemical evidence Geological Society of America Bulletin 87 725–737.2.0.CO;2>CrossRefGoogle Scholar
Huang, C. Retallack, G.J. and Wang, C., 2010 Cretaceous calcareous paleosols: pedogenetic characteristics and paleoenvironmental implications Acta Pedologica Sinica 47 1029–1038.Google Scholar
Huang, C. Retallack, G.J. Wang, C. and Huang, Q., 2013 Paleoatmospheric pCO2 fluctuations across the Cretaceous—Tertiary boundary recorded from paleosol carbonatesin NE China Palaeogeography, Palaeoclimatology, Palaeoecology 385 95–105.CrossRefGoogle Scholar
Huang, W.-L. Longo, J.M. and Pevear, D.R., 1993 An experimentally derived kinetic model for smectite-to-illite conversion and its use as a geothermometer Clays and Clay Minerals 41 162–177.CrossRefGoogle Scholar
Khidir, A. and Catuneanu, O., 2009 Basin-scale distribution of authigenic clay minerals in the late Maastrichtian—early Paleocene fluvial strata of the Alberta foredeep: Implications for burial depth Bulletin of Canadian Petroleum Geology 57 251–274.CrossRefGoogle Scholar
Li, J. Batten, D.J. and Zhang, Y., 2011 Palynological record from a composite core through Late Cretaceous—Early Paleocene deposits in the Songliao Basin, northeast China and its biostratigraphic implications Cretaceous Research 32 1–12.CrossRefGoogle Scholar
Liu, Y., 1985 Clay minerals of Late Cretaceous Songliao Basin and their sedimentary environment Acta Sedimentologica Sinica 3 131–139.Google Scholar
Liu, Z. Colin, C. Trentesaux, A. Blamart, D. Bassinot, F. Siani, G. and Sicre, M.A., 2004 Erosional history of the eastern Tibetan Plateau since 190 kyr ago: clay mineralogical and geochemical investigations from the southwestern South China Sea Marine Geology 209 1–18.CrossRefGoogle Scholar
Liu, Z. Colin, C. Li, X. Zhao, Y. Tuo, S. Chen, Z. Siringan, F.P. Liu, J.T. Huang, C.-Y. You, C.-F. and Huang, K.-F., 2010 Clay mineral distribution in surface sediments of the northeastern South China Sea and surrounding fluvial drainage basins: Source and transport Marine Geology 277 48–60.CrossRefGoogle Scholar
Moore, D.M. and Reynolds, R.C., 1997 X-ray Diffraction and the Identification and Analysis of Clay Minerals 2nd edition New York Oxford University Press Inc..Google Scholar
Osborn, S.G. Duffield, L.T. Elliott, W.C. Wampler, J.M. Elmore, R.D. and Engel, M.H., 2014 The timing of diagenesis and thermal maturation of the Cretaceous Marias River shale, Disturbed Belt, Montana Clays and Clay Minerals 62 112–125.CrossRefGoogle Scholar
Peltonen, C. Marcussen, Bjørlykke, K. and Jahren, J., 2009 Clay mineral diagenesis and quartz cementation in mudstones: The effects of smectite to illite reaction on rock properties Marine and Petroleum Geology 26 887–898.CrossRefGoogle Scholar
Petschick, R. Kuhn, G. and Gingele, F., 1996 Clay mineral distribution in surface sediments of the South Atlantic: sources, transport, and relation to oceanography Marine Geology 130 203–229.CrossRefGoogle Scholar
Pytte, A. Reynolds, R.C., Naeser, N.D. and McCulloh, T.H., 1988 The thermal transformation of smectite to illite Thermal History of Sedimentary Basins Berlin Springer-Verlag.Google Scholar
Ren, J. Tamaki, K. Li, S. and Junxia, Z., 2002 Late Mesozoic and Cenozoic rifting and its dynamic setting in eastern China and adjacent areas Tectonophysics 344 175–205.CrossRefGoogle Scholar
Ren, Z. Xiao, D. and Chi, Y., 2001 Restoration of the palaeogeotherm in Songliao Basin Petroleum Geology and Oilfield Development in Daqing 20 13–14.Google Scholar
Robert, C. and Kennett, J.P., 1994 Antarctic subtropical humid episode at the Paleocene—Eocene boundary: Claymineral evidence Geology 22 211–214.2.3.CO;2>CrossRefGoogle Scholar
Sáez, A. Inglès, M. Cabrera, L. and de las Heras, A., 2003 Tectonic—palaeoenvironmental forcing of clay-mineral assemblages in nonmarine settings: The Oligocene—Miocene As Pontes Basin (Spain) Sedimentary Geology 159 305–324.CrossRefGoogle Scholar
Scott, R.W. Wan, X. Wang, C. and Huang, Q., 2012 Late Cretaceous chronostratigraphy (Turonian—Maastrichtian): Sk1 core Songliao Basin, China Geoscience Frontiers 3 357–367.CrossRefGoogle Scholar
Singer, A., 1984 The paleoclimatic interpretation of clay minerals in sediments — a review Earth-Science Reviews 21 251–293.CrossRefGoogle Scholar
Song, Z. Qin, Y. George, S.C. Wang, L. Guo, J. and Feng, Z., 2013 A biomarker study of depositional paleoenvironments and source inputs for the massive formation of Upper Cretaceous lacustrine source rocks in the Songliao Basin, China Palaeogeography, Palaeoclimatology, Palaeoecology 385 137–151.CrossRefGoogle Scholar
Środoń, J., 1999 Nature of mixed-layer clays and mechanisms of their formation and alteration Annual Review of Earth and Planetary Sciences 27 19–53.CrossRefGoogle Scholar
Środoń, J. Clauer, N. Huff, W. Dudek, T. and Banaś, M., 2009 K-Ar dating of the lower Palaeozoic K-bentonites from the Baltic Basin and the Baltic Shield: Implications for the role of temperature and time in the illitization of smectite Clay Minerals 44 361–387.CrossRefGoogle Scholar
Środoń, J. Paszkowski, M. Drygant, D. Anczkiewicz, A. and Banaś, M., 2013 Thermal history of Lower Paleozoic rocks on the peri-Tornquist margin of the east European craton (Podolia, Ukraine) inferred from combined XRD, K-Ar, and ATF data Clays and Clay Minerals 61 107–17732.CrossRefGoogle Scholar
Sun, S. Shu, L. Zeng, Y. Cao, J. and Feng, Z., 2007 Porosity—permeability and textural heterogeneity of reservoir sandstones from the lower Cretaceous Putaohua Member of Yaojia Formation, Weixing Oilfield, Songliao Basin, northeast China Marine and Petroleum Geology 24 109–127.CrossRefGoogle Scholar
Suresh, N. Ghosh, S.K. Kumar, R. and Sangode, S., 2004 Clay-mineral distribution patterns in late Neogene fluvial sediments of the Subathu sub-basin, central sector of Himalayan foreland basin: Implications for provenance and climate Sedimentary Geology 163 265–278.CrossRefGoogle Scholar
Thiry, M., 2000 Palaeoclimatic interpretation of clay minerals in marine deposits: An outlook from the continental origin Earth-Science Reviews 49 201–221.CrossRefGoogle Scholar
Vanderaveroet, P. and Deconinck, J.F., 1997 Clay mineralogy of Cenozoic sediments of the Atlantic city Borehole, New Jersey Proceedings of the Ocean Drilling Program, Scientific Results 150X 49–57.Google Scholar
Velde, B. and Vasseur, G., 1992 Estimation of the diagenetic smectite-to-illite transformation in time-temperature space American Mineralogist 77 967–976.Google Scholar
Wan, X. Zhao, J. Scott, R.W. Wang, P. Feng, Z. Huang, Q. and Xi, D., 2013 Late Cretaceous stratigraphy, Songliao Basin, NE China: Sk1 cores Palaeogeography, Palaeoclimatology, Palaeoecology 385 31–43.CrossRefGoogle Scholar
Wang, C.S. Feng, Z.Q. Wu, H.Y. Wang, P.J. Feng, Z.H. and Ren, Y.G., 2008 Preliminary achievement of the Chinese Cretaceous Continental Scientific Drilling Project — SK-I Acta Geologica Sinica 82 9–20.Google Scholar
Wang, C. Feng, Z. Zhang, L. Huang, Y. Cao, K. Wang, P. and Zhao, B., 2013 Cretaceous paleogeography and paleoclimate and the setting of SKI borehole sites in Songliao basin, northeast China Palaeogeography, Palaeoclimatology, Palaeoecology 385 17–30.CrossRefGoogle Scholar
Wang, C. Scott, R.W. Wan, X. Graham, S.A. Huang, Y. Wang, P. Wu, H. Dean, W.E. and Zhang, L., 2013 Late Cretaceous climate changes recorded in Eastern Asian lacustrine deposits and North American Epieric Sea strata Earth-Science Reviews 126 275–299.CrossRefGoogle Scholar
Wang, D.P. Liu, Z.J. and Liu, L., 1994 Evolution of Songliao Basin and Fluctuation of the Sealevel Beijing (in Chinese) Geological Publishing House.Google Scholar
Wang, G. Cheng, R. Wang, P. and Gao, Y., 2008 The forming mechanism of dolostone of Nengjiang Formation in Songliao Basin — Example from CCSD-SK Acta Geologica Sinica 82 2 48–54.Google Scholar
Wang, X. Xin, G. and Feng, Y., 1990 Study on clay mineralogy of the Songliao Basin Harbin, China (in Chinese) Heilongjiang Science and Technology Press.Google Scholar
Wilkinson, M. Haszeldine, R.S. and Fallick, A.E., 2006 Jurassic and Cretaceous clays of the northern and central North Sea hydrocarbon reservoirs reviewed Clay Minerals 41 151–186.CrossRefGoogle Scholar
Wilson, M.D. and Pittman, E.D., 1977 Authigenic clays in sandstones; recognition and influence on reservoir properties and paleoenvironmental analysis Journal of Sedimentary Research 47 3–31.Google Scholar
Wilson, M.J. Wilson, L. and Patey, I., 2014 The influence of individual clay minerals on formation damage of reservoir sandstones: A critical review with some new insights Clay Minerals 49 147–164.CrossRefGoogle Scholar
Wu, H. Zhang, S. Jiang, G. Hinnov, L. Yang, T. Li, H. Wan, X. and Wang, C., 2013 Astrochronology of the early Turonian—early Campanian terrestrial succession in the Songliao Basin, northeastern China and its implication for long-period behavior of the solar system Palaeogeography, Palaeoclimatology, Palaeoecology 385 55–70.CrossRefGoogle Scholar
Wu, H.C. Zhang, S.H. Hinnov, L.A. Jiang, G.Q. Yang, T.S. Li, H. Y. Wan, X.Q. and Wang, C.S., 2015 Cyclostratigraphy and orbital tuning of the terrestrial upper Santonian—Lower Danian in Songliao Basin, northeastern China Earth and Planetary Science Letters 407 82–95.CrossRefGoogle Scholar
Xiang, C. Feng, Z. Pang, X. Wu, H. and Li, J., 2007 Late stage thermal history of the Songliao Basin and its tectonic implications: Evidence from apatite fission track (AFT) analyses Science in China Series D: Earth Sciences 50 1479–1487.CrossRefGoogle Scholar