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Diagenesis of Dioctahedral and Trioctahedral Smectites from Alternating Beds in Miocene to Pleistocene Rocks of the Niigata Basin, Japan

Published online by Cambridge University Press:  28 February 2024

Byeong-Kook Son ,
Takahisa Yoshimura  and
Hikaru Fukasawa
Byeong-Kook Son
Affiliation:
Korea Institute of Geoscience and Mineral Resources (KIGAM), 30, Kajungdong, Yusungku, Taejon, Korea
Takahisa Yoshimura*
Affiliation:
Department of Environmental Sciences, Faculty of Sciences, Niigata University, Ikarashi-2, Niigata, Japan
Hikaru Fukasawa
Affiliation:
Exploration Department, Japan Petroleum Exploration Co. Ltd, Higashi-Shinagawa, Tokyo, Japan
*
*Present address: 7910-22, 2-No-Cho, Ikarashi, Niigata, Japan.
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Abstract

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Clay mineral diagenesis in the Niigata basin is documented by mineralogical and chemical analysis of clay minerals from cuttings from the Shinkumoide SK-1D (SSK-1D) well which is characterized by alternating beds containing dioctahedral and trioctahedral smectite minerals with increasing depth. Dioctahedral smectite shows a progressive increase in illite interstratification with increasing depth. The transition of dioctahedral smectite to interstratified illite-smectite (I-S) is supported chemically by an increase in K and Al and a decrease in Si with increasing depth. In contrast, trioctahedral smectite (saponite) reacts to form a 1:1 interstratified chlorite-smectite (C-S) with increasing burial depth and temperature. Considering the geology and the occurrence of smectite, the SSK-1D smectites probably altered diagenetically from two different parent materials: dioctahedral smectite is derived from clastic sediments and transforms to interstratified illite-smectite, whereas trioctahedral smectite is derived from andesitic pyroclastic rocks and transforms to interstratified chlorite-smectite.

The C-S occurs at the same depth of ~3200 m as the conversion of randomly interstratified (R = 0) I-S to (R = 1) I-S. Furthermore, the depth is compatible with a Tmax temperature of 430-435°C, which indicates the starting temperature for oil generation from organic matter. The temperature of the conversion of (R = 0) I-S to (R = 1) I-S and the start of corrensite formation is estimated at 110-120°C based on the time-temperature model suggested by others. The clay-mineral diagenesis in the SSK-1D further suggests that I-S and C-S can act as geothermometers in clastic and pyroclastic sediments provided that the effect of time is considered.

Keywords

Chlorite-SmectiteClay Mineral DiagenesisC-SGeothermometerIllite-SmectiteI-SNiigata BasinSaponite
Type
Research Article
Information
Clays and Clay Minerals , Volume 49 , Issue 4 , August 2001 , pp. 333 - 346
Copyright
Copyright © 2001, The Clay Minerals Society

References

Altaner, S. P. and Ylagan, R. F., 1997 Comparison of structural models of mixed-layer illite/smectite and reaction mechanisms of smectite illitization Clays and Clay Minerals 45 517–533 10.1346/CCMN.1997.0450404.CrossRefGoogle Scholar
Badaut, D. Besson, G. Decarreau, A. and Rautureau, R., 1985 Occurrence of a ferrous, trioctahedral smectite in recent sediments of Atlantis II Deep, Red Sea Clay Minerals 20 389–404 10.1180/claymin.1985.020.3.09.CrossRefGoogle Scholar
Beaufort, D. Baronnet, A. Lanson, B. and Meunier, A., 1997 Corrensite: A single phase or a mixed-layer phyllo-silicate in the saponite-to-chlorite conversion series? A case study of Sancerre-Couy deep drill hole (France) American Mineralogist 82 109–124 10.2138/am-1997-1-213.CrossRefGoogle Scholar
Burtner, R. L. and Warner, M. A., 1986 Relationship between illite/smectite diagenesis and hydrocarbon generation in Lower Cretaceous Mowry and Skull Creek shales of the northern Rocky Mountain area Clays and Clay Minerals 34 390–402 10.1346/CCMN.1986.0340406.CrossRefGoogle Scholar
Chang, H. K. Mackenzie, F. T. and Schoonmaker, J., 1986 Comparisons between the diagenesis of dioctahedral and trioctahedral smectite, Brazilian offshore basins Clays and Clay Minerals 34 407–423 10.1346/CCMN.1986.0340408.CrossRefGoogle Scholar
Elliott, W. C. Aronson, J. L. Matisoff, G. and Gautier, D. L., 1991 Kinetics of the smectite to illite transformation in the Denver basin: Clay mineral, K-Ar data, and mathematical model results American Association of Petroleum Geologists Bulletin 75 436–462.Google Scholar
Eslinger, E. and Pevear, D., 1988 Clay Minerals for Petroleum Geologists and Engineers. 10.2110/scn.88.22.CrossRefGoogle Scholar
Espitalié, J. Deroo, G. and Marquis, F., 1985 La pyrolyse Rock Eval et ses applications Revue de l’Institute Français du Petrole 40 563–784 10.2516/ogst:1985035.CrossRefGoogle Scholar
Hillier, S., 1993 Origin, diagenesis, and mineralogy of chlorite minerals in Devonian lacustrine mudrocks, Orcadian basin, Scotland Clays and Clay Minerals 41 240–259 10.1346/CCMN.1993.0410211.CrossRefGoogle Scholar
Hoffman, J. Hower, J., Scholle, P. A. and Schluger, P. S., 1979 Clay mineral assemblages as low grade metamorphic geothermometers: Application to the thrust faulted disturbed belt of Montana Aspects of Diagenesis 55–79 10.2110/pec.79.26.0055.CrossRefGoogle 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 American Bulletin 87 125–737 10.1130/0016-7606(1976)87<725:MOBMOA>2.0.CO;2.2.0.CO;2>CrossRefGoogle Scholar
Iijima, A. Utada, M. and Gould, R. F., 1971 Present-day zeolitic diagenesis of the Neogene geosynclinal deposits in the Niigata oilfield, Japan Molecular Sieve Zeolite-I 342–349.CrossRefGoogle Scholar
Inoue, A., Shultz, L. G. van Olphen, H. and Mumpton, F. A., 1987 Conversion of smectite to chlorite by hydro-thermal and diagenetic alterations, Hokuroku kuroko mineralization area, Northeast Japan Proceedings of the International Clay Conference, Denver 1985 158–164.CrossRefGoogle Scholar
Inoue, A. and Utada, M., 1983 Further investigations of a conversion series of dioctahedral mica/smectites in the Shinzan hydrothermal alteration area, northeast Japan Clays and Clay Minerals 31 401–412 10.1346/CCMN.1983.0310601.CrossRefGoogle Scholar
Inoue, A. and Utada, M., 1991 Smectite-to-chlorite transformation in thermally metamorphosed vocanoclastic rocks in the Kimikita area, northern Honshu, Japan American Mineralogist 76 628–640.Google Scholar
Inoue, A. Kohyama, N. Kitagawa, R. and Watanabe, T., 1987 Chemical and morphological evidence for the conversion of smectite to illite Clays and Clay Minerals 35 115–120 10.1346/CCMN.1987.0350203.CrossRefGoogle Scholar
Kimbara, K., 1975 Contributions to Clay Mineralogy. .Google Scholar
Kobayashi, I. and Yoshimura, T., 2000 Explanatory text of the Niigata geological map. .Google Scholar
Kobayashi, I. Tateishi, M. Yoshioka, T. and Shimazu, M., 1991 Geology of the Nagaoka District. .Google Scholar
Moore, D. M. and Reynolds, R. C., 1989 X-ray Diffraction and the Identification and Analysis of Clay Minerals. .Google Scholar
Nadeau, P. H. Wilson, M. J. McHardy, W. J. and Tait, J. M., 1984 Interparticle diffraction: A new concept for inter-stratified clays Clay Minerals 19 757–769 10.1180/claymin.1984.019.5.06.CrossRefGoogle Scholar
Niu, B. and Yoshimura, T., 1996 Smectite conversion in dia-genesis and low grade hydrothermal alteration from Neo-gene basaltic marine sediments in Niigata Basin, Japan Clay Science 10 37–56.Google Scholar
Niu, B. Yoshimura, T. and Hirai, A., 2000 Smectite diagen-esis in Neogene marine sandstone and mudstone of the Niigata basin, Japan Clays and Clay Minerals 48 26–42 10.1346/CCMN.2000.0480104.CrossRefGoogle Scholar
Perry, E. A. and Hower, J., 1972 Late-stage dehydration in deeply buried pelitic sediments American Association of Petroleum Geologists Bulletin 56 2013–2021.Google Scholar
Pollastro, R. M., 1985 Mineralogical and morphological evidence for the formation of illite at the expense of illite/smectite Clays and Clay Minerals 33 265–274 10.1346/CCMN.1985.0330401.CrossRefGoogle Scholar
Pollastro, R. M., 1993 Considerations and applications of the illite/smectite geothermometer in hydrocarbon-bearing rocks of Miocene to Mississippian age Clays and Clay Minerals 41 119–133 10.1346/CCMN.1993.0410202.CrossRefGoogle Scholar
Pytte, A. M. Reynolds, R. C., Naeser, N. D. and McCulloh, T. H., 1989 The thermal transformation of smectite to illite Thermal History of Sedimentary Basins 133–140 10.1007/978-1-4612-3492-0_8.CrossRefGoogle Scholar
Reynolds, R. C. Jr, 1985 NEWMOD: A computer program for the calculation of the one-dimensional patterns of mixed-layered clays. .Google Scholar
Sato, X. Kudo, X. and Kameo, K., 1995 On the distribution of source rocks in the Niigata oil field based on the micro-fossil biostratigraphy Journal of the Japanese Association for Petroleum Technology 60 76–86 10.3720/japt.60.76.CrossRefGoogle Scholar
Shau, Y -H Peacor, D. R. and Essene, E. J., 1990 Corrensite and mixed-layer chlorite/corrensite in metabasalt from northern Taiwan: TEM/AEM, EPMA, XRD, and optical studies Contributions to Mineralogy and Petrology 105 123–142 10.1007/BF00678980.CrossRefGoogle Scholar
Sietronic., 1996 SIROQUANT: A quantitative XRD software. .Google Scholar
Son, B -K and Yoshimura, T., 1997 The smectite-to-illite transition in the Koyoshigawaoki well in the Akita sedimentary basin, Northeast Japan Clay Science 10 163–183.Google Scholar
Środoń, J. Eberl, D. D. and Bailey, S. W., 1984 Illite Micas 495–544 10.1515/9781501508820-016.CrossRefGoogle Scholar
Sudo, T., 1954 Iron-rich saponite found from Tertiary iron sand beds of Japan Journal of Geological Society of Japan 60 18–27 10.5575/geosoc.60.18.Google Scholar
Yoshimura, T., 1983 Neoformation and transformation of trioctahedral clay minerals in diagenetic process Journal of Sedimentology of Japan .Google Scholar