Abstract
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.
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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.
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.
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.
Chamley, H. (1989) Clay Sedimentology. Springer Verlag, Berlin, 623 pp.
Chen, P. and Chang, Z. (1994) Nonmarine Cretaceous stratigraphy of eastern China. Cretaceous Research, 15, 245–257.
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 (in Chinese with English abstract).
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 (in Chinese with English abstract).
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.
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.
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.
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.
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.
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.
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.
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.
Elliott, W.C. and Matisoff, G. (1996) Evaluation of kinetic models for the smectite to illite transformation. Clays and Clay Minerals, 44, 77–87.
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.
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.
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.
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.
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 (in Chinese with English abstract).
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. Geological Publishing House, Beijing (in Chinese).
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.
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.
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.
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 (in Chinese with English abstract).
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.
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.
Hou, Q.J., Feng, Z.Q., and Feng, Z.H. (2009) Terrestrial Petroleum Geology of Songliao Basin. Petroleum Industry Press, Beijing (in Chinese).
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.
Huang, C., Retallack, G.J., and Wang, C. (2010) Cretaceous calcareous paleosols: pedogenetic characteristics and paleoenvironmental implications. Acta Pedologica Sinica, 47, 1029–1038.
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.
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.
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.
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.
Liu, Y. (1985) Clay minerals of Late Cretaceous Songliao Basin and their sedimentary environment. Acta Sedimentologica Sinica, 3, 131–139 (in Chinese with English abstract).
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.
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.
Moore, D.M. and Reynolds, R.C. (1997) X-ray Diffraction and the Identification and Analysis of Clay Minerals, 2nd edition. Oxford University Press Inc., New York.
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.
Peltonen, C., Marcussen, Ø., 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.
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.
Pytte, A. and Reynolds, R.C. (1988) The thermal transformation of smectite to illite. Pp. 133–140 in: Thermal History of Sedimentary Basins (N.D. Naeser and T.H. McCulloh, editors). Springer-Verlag, Berlin.
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.
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 (in Chinese with English abstract).
Robert, C. and Kennett, J.P. (1994) Antarctic subtropical humid episode at the Paleocene—Eocene boundary: Claymineral evidence. Geology, 22, 211–214.
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.
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.
Singer, A. (1984) The paleoclimatic interpretation of clay minerals in sediments — a review. Earth-Science Reviews, 21, 251–293.
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.
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.
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.
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.
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.
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.
Thiry, M. (2000) Palaeoclimatic interpretation of clay minerals in marine deposits: An outlook from the continental origin. Earth-Science Reviews, 49, 201–221.
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, 150 X, 49–57.
Velde, B. and Vasseur, G. (1992) Estimation of the diagenetic smectite-to-illite transformation in time-temperature space. American Mineralogist, 77, 967–976.
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.
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 (in Chinese with English abstracts).
Wang, C., Feng, Z., Zhang, L., Huang, Y., Cao, K., Wang, P., and Zhao, B. (2013a) Cretaceous paleogeography and paleoclimate and the setting of SKI borehole sites in Songliao basin, northeast China. Palaeogeography, Palaeoclimatology, Palaeoecology, 385, 17–30.
Wang, C., Scott, R.W., Wan, X., Graham, S.A., Huang, Y., Wang, P., Wu, H., Dean, W.E., and Zhang, L. (2013b) Late Cretaceous climate changes recorded in Eastern Asian lacustrine deposits and North American Epieric Sea strata. Earth-Science Reviews, 126, 275–299.
Wang, D.P., Liu, Z.J., and Liu, L. (1994) Evolution of Songliao Basin and Fluctuation of the Sealevel. Geological Publishing House, Beijing (in Chinese).
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 (in Chinese with English abstract).
Wang, X., Xin, G., and Feng, Y. (1990) Study on clay mineralogy of the Songliao Basin. Heilongjiang Science and Technology Press, Harbin, China (in Chinese).
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.
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.
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.
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.
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.
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.
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Gao, Y., Wang, C., Liu, Z. et al. Diagenetic and Paleoenvironmental Controls on Late Cretaceous Clay Minerals in the Songliao Basin, Northeast China. Clays Clay Miner. 63, 469–484 (2015). https://doi.org/10.1346/CCMN.2015.0630605
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DOI: https://doi.org/10.1346/CCMN.2015.0630605