Hostname: page-component-586b7cd67f-2brh9 Total loading time: 0 Render date: 2024-12-03T19:09:13.878Z Has data issue: false hasContentIssue false

Sandstone composition of the Upper Jurassic Emuerhe Formation from the Mohe Basin, China

Published online by Cambridge University Press:  27 November 2013

MING MING ZHANG
Affiliation:
College of Earth Science, Jilin University, Changchun 130061, China
ZHAO JUN LIU*
Affiliation:
College of Earth Science, Jilin University, Changchun 130061, China
SHI FANG
Affiliation:
College of Earth Science, Jilin University, Changchun 130061, China
QIU SHI SUN
Affiliation:
College of Earth Science, Jilin University, Changchun 130061, China
*
*Author for correspondence: [email protected]

Abstract

The sandstone composition analysis carried out on the samples from three different sections (western section, middle section and eastern section) of the Upper Jurassic Emuerhe Formation in the Mohe Basin, northeastern China, reveals that the Okhotsk orogenic belt and the Ergun massif basement are the source areas for the Emuerhe Formation. The source area of the western section and the A segment of the middle section is the Okhotsk orogenic belt. The tectonic attributes of the Okhotsk orogenic belt are those of a dissected arc. The transportation distance of clastic rocks from these sections gradually lengthened, and the uplift rate of the Okhotsk orogenic belt gradually increased. The source area of the eastern section and the B segment of the middle section is the Ergun massif basement. Compared with the Okhotsk orogenic belt, the tectonic attributes and uplift rate of the Ergun massif basement are different from the former. The attributes of the Ergun massif basement are those of basement uplift. The transportation distance of clastic rocks from the eastern section and the B segment of the middle section gradually shortened, and the uplift rate of the Ergun massif basement gradually decreased. These conclusions are consistent with the characteristics of a foreland basin. Thus, we can draw the conclusion that the Mohe Basin belongs to the foreland basin.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 2013 

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Biao, S. H., Zheng, W. Z. & Zhou, X. F. 2012. Zircon U-Pb age of the North Da Hinggan Mts., NE China and its constraint to attribute of the Erguna Block. Acta Geologica Sinica 86, 1262–71 (in Chinese with English abstract).Google Scholar
Caracciolo, L., Le Pera, E., Muto, F. & Perri, F. 2011. Sandstone petrology and mudstone geochemistry of the Peruc-Korycany Formation (Bohemian Cretaceous Basin, Czech Republic). International Geology Review 53, 1003–31.Google Scholar
Chang, L. H., Wang, X. Y., Wang, X. Z., Zhao, B. X. & Liang, H. J. 2007. Characteristics and evolution of thrust nappe structure in the Mohe Area, Daxing'anling. Journal of Jilin University (Earth Science Edition) 37, 11–5 (in Chinese with English abstract).Google Scholar
Critelli, S. & Ingersoll, R. V. 1994. Sandstone petrology and provenance of the Siwalik Group (northwestern Pakistan and western-southeastern Nepal). Journal of Sedimentary Research 64, 815–23.Google Scholar
Critelli, S. & Ingersoll, R. V. 1995. Interpretation of neovolcanic versus palaeovolcanic sand grains: an example from Miocene deep-marine sandstone of the Topanga Group (southern California). Sedimentology 42, 783804.CrossRefGoogle Scholar
Critelli, S., Mongelli, G., Perri, F., Martín-Algarra, A., Martín-Martín, M., Perrone, V., Dominici, R., Sonnino, M. & Zaghloul, M. N. 2008. Compositional and geochemical signatures for the sedimentary evolution of the Middle Triassic–Lower Jurassic continental redbeds from Western-Central Mediterranean Alpine chains. Journal of Geology 116, 375–86.CrossRefGoogle Scholar
Critelli, S., Muto, F., Tripodi, V. & Perri, F. 2013. Link between thrust tectonics and sedimentation processes of stratigraphic sequences from the southern Apennines foreland basin system, Italy. Rendiconti Online della Società Geologica Italiana 25, 2142.Google Scholar
Crosdale, P. J., Sorokin, A. P., Woolfe, K. J. & Macdonald, D. I. M. 2002. Inertinite-rich Tertiary coals from the Zeya–Bureya Basin, Far Eastern Russia. International Journal of Coal Geology 51, 215–35.Google Scholar
Dickinson, W. R. 1985. Interpreting provenance relations from detrital modes of sandstones. In Provenance of Arenites (ed. Zuffa, G. G.), pp. 333–61. Dordrecht: Reidel.Google Scholar
Dickinson, W. R. 1988. Provenance and sediment dispersal in relation to paleotectonics and paleogeography of sedimentary basins. In New Perspectives in Basin Analysis (eds Kleinspehn, K. L. & Paola, C.), pp. 326. Springer.Google Scholar
Dickinson, W. R., Beard, L. S., Brakeniridge, G. R., Erjavec, J. L., Ferguson, R. C., Inman, K. F., Knepp, R. A., Lindberg, F. A. & Ryberg, P. T. 1983. Provenance of North American Phanerozoic sandstones in relation to tectonic setting. Geological Society of America Bulletin 94, 222–35.2.0.CO;2>CrossRefGoogle Scholar
Dickinson, W. R. & Suczek, C. A. 1979. Plate tectonics and sandstone compositions. American Association of Petroleum Geologists Bulletin 63, 2164–82.Google Scholar
Fang, S. H., Guo, S. J., Wu, C. D., Zhang, Z. C., Wang, M. N. & Yuan, Q. D. 2006. Jurassic clastic composition in the Southern Junggar Basin, Northwest China: implications for basin-range pattern and tectonic attributes. Acta Geologica Sinica 80, 196209 (in Chinese with English abstract).Google Scholar
Fang, S. H., Jia, C. Z., Song, Y., Guo, Z. J., Yuan, S. W. & Wang, X. L. 2007 a. Meso-Cenozoic tectonic events and structural constraints in the Southern Junggar basin: evidence from detrital compositions. Chinese Journal of Geology 81, 753–65 (in Chinese with English abstract).Google Scholar
Fang, S. H., Song, Y., Jia, C. Z., Wang, X. L. & Yuan, Q. D. 2007 b. The Mesozoic-Cenozoic clastic composition of Bogda Area, Xinjiang: implications on the evolution of basin-range pattern. Acta Geologica Sinica 81, 1229–37 (in Chinese with English abstract).Google Scholar
Folk, R. L. 1974. Petrology of Sedimentary Rocks. Austin, Texas: Hemphill's, 182 pp.Google Scholar
Ge, W. C., Sui, Z. M., Wu, F. Y., Zhang, J. H. & Xu, X. C. 2007. Zircon U-Pb ages, Hf isotopic characteristics and their implications of the Early Paleozoic granites in the northeastern Da Hinggan Mts., northeastern China. Acta Petrologica Sinica 23, 423–40 (in Chinese with English abstract).Google Scholar
Ge, W. C., Wu, F. Y., Zhou, C. Y. & Rahman, A. A. A. 2005. Emplacement age of the Tahe granite and its constraint on the tectonic nature of the Erguna block in the northern part of the Daxing an Range. Chinese Science Bulletin 50, 1239–47 (in Chinese with English abstract).Google Scholar
Ghazi, S. & Mountney, N. P. 2011. Petrography and provenance of the Early Permian Fluvial Warchha Sandstone, Salt Range, Pakistan. Sedimentary Geology 233, 88110.Google Scholar
Graham, S. A., Hendrix, M. S., Wang, L. B. & Carrol, A. R. 1993. Collision successor basin of western China: impact of tectonic inheritance on sand composition. Geological Society of America Bulletin 105, 323–44.Google Scholar
Gray, M. B. & Zeitler, P. K. 1997. Comparison of clastic wedge provenance in the Appalachian foreland using U-Pb ages of detrital zircons. Tectonics 16, 151–60.Google Scholar
He, Z. J., Li, J. T., Mo, S. G. & Sorokin, A. A. 2003. Tectonic setting of geochemical characteristics and provenance analysis of the sandstones in Mohe foreland basin. Science in China (Series D) 33, 1219–26 (in Chinese with English abstract).Google Scholar
He, Z. H., Wang, Y. F. & Hou, W. 2008. Geochemistry and provenance analysis of the Middle Jurassic sandstones in the Mohe Basin, Heilongjiang. Sedimentary Geology and Tethyan Geology 28, 93100 (in Chinese with English abstract).Google Scholar
Hendrix, M. S. 2000. Evolution of Mesozoic sandstone compositions, southern Junggar, northern Tarim, and western Tumpan basin northwest China: a detrital record of the ancestral Tian Shan. Journal of Sedimentary Research 70, 520–32.Google Scholar
Hendrix, M. S., Granham, S. A., Carroll, A. R., Soble, E. R., Mcnight, C. L., Schlein, B. J. & Wang, Z. X. 1992. Sedimentary record and climatic implications of recurrent deformation in the Tian Shan: evidence from Mesozoic strata of the north Tarim, south Junggar, and Turpan basins, northwest China. Geological Society of America Bulletin 104, 5379.Google Scholar
Hou, W., Liu, Z. J., He, Y. P., He, Z. H. & Zhang, L. 2010 a. Provenance analysis of Middle Jurassic sediments and its geological significance in Mohe Basin. Journal of Jilin University (Earth Science Edition) 40, 286–97 (in Chinese with English abstract).Google Scholar
Hou, W., Liu, Z. J., He, Y. P., He, Z. H., Zhang, Y. Q. & Zhang, L. 2010 b. Provenance analysis of Upper Jurassic and its geological significances in Mohe Basin. Geological Review 56, 71–9 (in Chinese with English abstract).Google Scholar
Ingersoll, R. V. 1988. Tectonics of sedimentary basins. Geological Society of America Bulletin 100, 1704–19.Google Scholar
Ingersoll, R. V., Fullard, T. F., Ford, R. L., Grimm, J. P., Pickle, J. D. & Sares, S. W. 1984. The effect of grain size on detrital modes: a test of the Gazzi-Dickinson point counting method. Journal of Sedimentary Petrology 54, 103–16.Google Scholar
Ingersoll, R. V. & Suczek, C. A. 1979. Petrology and provenance of Neogene sand from Nicobar and Bengal fans. DSDP sites 211 and 218. Journal of Sedimentary Petrology 49, 1217–28.Google Scholar
Lee, Y. I. & Sheen, D. H. 1998. Detrital modes of the Pyeongan Supergroup (Late Carboniferous–Early Triassic) sandstones in the Samcheog coalfield, Korea: implications for provenance and tectonic setting. Sedimentary Geology 119, 219–38.Google Scholar
Li, C. L. 2007. Structural characteristic, tectonic evolution and basin dynamics of Mohe Basin. Ph.D. thesis, College of Earth Science, China University of Geosciences, Beijing. Published thesis. pp. 24–45 (in Chinese with English abstract).Google Scholar
Li, Z., Song, W. J., Peng, S, T., Wang, D. X. & Zhang, Z. P. 2004 a. Mesozoic– Cenozoic tectonic relationships between the Kuqa subbasin and Tian Shan, northwest China: constraints from depositional records. Sedimentary Geology 172, 223–49.Google Scholar
Li, Z., Wang, D. X., Lin, W. & Wang, Q. C. 2004 b. Mesozoic-Cenozoic clastic composition in Kuqa depression, northwest China: implication for provenance types and tectonic attributes. Acta Petrologica Sinica 20, 655–66 (in Chinese with English abstract).Google Scholar
Lin, C. S., Yang, H. J., Liu, J. Y., Rui, Z. F., Cai, Z. Z. & Zhu, Y. F. 2012. Distribution and erosion of the Paleozoic tectonic unconformities in the Tarim Basin, Northwest China: significance for the evolution of paleo-uplifts and tectonic geography during deformation. Journal of Asian Earth Sciences 46, 119.Google Scholar
Liu, Y. Q., Wang, Z. X., Jin, X. C., Li, T. & Li, Y. 2004. Evolution, chronology and depositional effect of uplifting in the eastern sector of the Tianshan Mountains. Acta Geologica Sinica 78, 319–31 (in Chinese with English abstract).Google Scholar
Lu, F. X. & Sang, L. 2002. Geological. pp. 162–78. Geological Publishing House of Beijing, Special Publication no. 116 (in Chinese).Google Scholar
Marenssi, S. A., Net, L. I. & Santillana, S. N. 2002. Provenance, environmental and paleogeographic controls on sandstone composition in an incised-valley system: the Eocene La Meseta Formation, Seymour Island, Antarctica. Sedimentary Geology 150, 301–21.Google Scholar
Mo, S. G., Han, M. L. & Li, J. T. 2005. Compositions and orogenic processes of Mongolia-Okhotsk Orogen. Journal of Shandong University of Science and Technology (Natural Science) 24, 5064 (in Chinese with English abstract).Google Scholar
Morton, A. C. & Hallsworth, C. 1994. Identifying provenance specific features of detrital heavy mineral assemblages in sandstones. Sedimentary Geology 90, 241–56.Google Scholar
Perri, F., Cirrincione, R., Critelli, S., Mazzoleni, P. & Pappalardo, A. 2008. Clay mineral assemblages and sandstone compositions of the Mesozoic Longobucco Group (north-eastern Calabria): implication for burial history and diagenetic evolution. International Geology Review 50, 1116–31.CrossRefGoogle Scholar
Perri, F., Critelli, S., Cavalcante, F., Mongelli, G., Dominici, R., Sonnino, M. & De Rosa, R. 2012. Provenance signatures for the Miocene volcaniclastic succession of the Tufiti di Tusa Formation, southern Apennines, Italy. Geological Magazine 149, 423–42.CrossRefGoogle Scholar
Perri, F., Critelli, S., Martín-Algarra, A., Martín-Martín, M., Perrone, V., Mongelli, G. & Zattin, M. 2013. Triassic redbeds in the Malaguide Complex (Betic Cordillera – Spain): petrography, geochemistry, and geodynamic implications. Earth-Science Reviews 117, 128.CrossRefGoogle Scholar
Perri, F., Critelli, S., Mongelli, G. & Cullers, R. L. 2011. Sedimentary evolution of the Mesozoic continental redbeds using geochemical and mineralogical tools: the case of Upper Triassic to Lowermost Jurassic M.te di Gioiosa mudstones (Sicily, southern Italy). International Journal of Earth Sciences 100, 1569–87.Google Scholar
Rieser, A. B., Neubauer, F., Liu, Y. J. & Ge, X. H. 2005. Sandstone provenance of north-western sectors of the intracontinental Cenozoic Qaidam basin, western China: tectonic vs. climatic control. Sedimentary Geology 177, 118.Google Scholar
Shao, J. D., Tan, Q., Wang, H., Zhang, M. & He, H. Y. 2011. The Mesozoic strata and the Jurassic-Cretaceous boundary in the Daxinganling Region. Geology and Resources 20 (1), 411.Google Scholar
Sun, G. R., Li, Y. C. & Zhang, Y. 2002. The basement tectonics of Erguna massif. Geology and Resources 11, 129–39 (in Chinese with English abstract).Google Scholar
Wang, C. W., Sun, Y. W., Li, N., Zhao, G. W. & Ma, X. Q. 2009. Tectonic implications of Late Paleozoic stratigraphic distribution in Northeast China and adjacent region. Science in China (Series D) – Earth Science 52, 619–26.Google Scholar
Wu, G. Y., Feng, Z. Q., Yang, J. G., Wang, Z. J., Zhang, L. G. & Guo, Q. X. 2006. Tectonic setting and geological evolution of Mohe basin in Northeast China. Oil & Gas Geology 27, 528–35 (in Chinese with English abstract).Google Scholar
Wu, G., Sun, F. Y., Zhao, C. S., Li, Z. T., Zhao, A. L., Pang, Q. B. & Li, G. Y. 2005. Discovery of the Early Paleozoic post-collisional granites in northern margin of the Erguna massif and its geological significance. Chinese Science Bulletin 50, 2278–88 (in Chinese with English abstract).Google Scholar
Wu, H. Y., Wang, S. H. & Yang, J. G. 2004. Analysis of exploration potential in surrounding basins of Daqing Oilfield. China Petroleum Exploration 4, 2331 (in Chinese with English abstract).Google Scholar
Wu, H. Y., Yang, J. G., Huang, Q. H. & Liu, W. L. 2003. Sequence and age of the Mesozoic strata of Mohe Basin. Journal of Stratigraphy 27, 193–8 (in Chinese with English abstract).Google Scholar
Xie, M. Q. 2000. The cohesive slab structures and their driving mechanism–tectonics evolutions in the Northeast China and neighboring areas, pp. 66–70. Science Press of Beijing, Special Publication no. 134 (in Chinese).Google Scholar
Xin, R. C., Wu, H. Y. & Yang, J. G. 2003. Upper Jurassic sequence-stratigraphic framework of the Mohe Basin. Journal of Stratigraphy 27, 198204 (in Chinese with English abstract).Google Scholar
Xu, G. G. & Yan, H. Q. 1996. Accretionary tectonics in the Northeast of Russia. Global Geology 15, 35–8 (in Chinese).Google Scholar
Yan, Y., Lin, G., Wang, Y. J. & Guo, F. 2002. The indication of continental detrital sediment to tectonic setting. Advances in Earth Sciences 17, 8590 (in Chinese with English abstract).Google Scholar
Zaghloul, M. N., Critelli, S., Perri, F., Mongelli, G., Perrone, V., Sonnino, M., Tucker, M., Aiello, M. & Ventimiglia, C. 2010. Depositional systems, composition and geochemistry of Triassic rifted-continental margin redbeds of Internal Rif Chain, Morocco. Sedimentology 57, 312–50.Google Scholar
Zeng, Y. F. & Xia, W. J. 1998. Petrology, pp. 212–25. Geological Publishing House of Beijing, Special Publication no.112 (in Chinese).Google Scholar
Zhang, S., Lin, C. M., Wu, C. D. & Yang, J. G. 2003. Tectonic characteristics and basin evolution of the Mohe Basin, Heilongjiang Province. Geological Journal of China University 9, 411–8 (in Chinese with English abstract).Google Scholar