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Relationships between authigenic mineral transformation and variation in vitrinite reflectance during diagenesis: an example from the Tertiary of northern Kyushu, Japan

Published online by Cambridge University Press:  09 July 2018

T. Miki
Affiliation:
Department of Earth and Planetary Sciences, Kyushu University, Fukuoka 812, Japan
Y. Nakamuta
Affiliation:
Department of Earth and Planetary Sciences, Kyushu University, Fukuoka 812, Japan
J. Aizawa
Affiliation:
Department of Geology, Fukuoka University, Fukuoka 814-01, Japan

Abstract

The Tertiary sequences in northern Kyushu, Japan, contain several types of zeolite and clay minerals together with carbonaceous materials. A correlation between authigenic mineral zones and vitrinite reflectance reveals the delay in mineral authigenesis relative to the increase in vitrinite reflectance compared with similar studies in other regions. This may be ascribed to causes such as high paleogeothermal gradient, and chemical composition of pore-waters and host sediment.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1991

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References

Aoyagi, K. & Kazama, T. (1980) Transformational changes of clay minerals, zeolites and silica minerals during diagenesis. Sedimentology, 27, 179–188.Google Scholar
Bostick, N.H. (1973) Time as a factor in thermal metamorphism of phytoclasts (coaly particles). Compte Rendu Spec. vol., 183193.Google Scholar
Brooks, J. (1981) Organic maturation of sedimentary organic matter and petroleum exploration: a review. Pp. 137 in: Organic Maturation Studies and Fossil Fuel Exploration (Brooks, J., editor). Academic Press, London.Google Scholar
Castaño, J.R. & Sparks, D.M. (1974) Interpretation of vitrinite reflectance measurements in sedimentary rocks and determination of burial history using vitrinite reflectance and authigenic minerals. Pp. 3152 in: Carbonaceous Materials as Indicators of Metamorphism (Dutcher, R.R., Hacquebard, P.A., Schopf, J.M. & Simon, J.A., editors). Geol. Soc. Am. Spec. Pap., 153.Google Scholar
Coombs, D.S. (1954) The nature and alteration of some Triassic sediments from Southland, New Zealand. R. Soc. N.Z. Trans., 82, 65–109.Google Scholar
Dunoyer de Segonzac, G. (1970) The transformation of clay mineraJs during diagenesis and low-grade metamorphism: a review. Sedimentology, 15, 281–346.Google Scholar
Hood, A., Gutjahr, C.C.M. & Heacock, R.L. (1975) Organic metamorphism and the generation of petroleum. Am. Ass. Petrol. Geologists Bull., 59, 986–996.Google Scholar
Iijima, A. (1975) Effect of pore water to clinoptilolite-analcime-albite reaction series. J. Fac. Sci. Univ. Tokyo,, 19, 133–147.Google Scholar
Iijima, A. & Utada, M. (1971) Present-day zeolitic diagenesis of the Neogene geosynclinal deposits in the Niigata oil field, Japan. Adv. Chem. Ser., 101, 342–349.Google Scholar
Kisch, H.J. (1969) Coal-rank and burial-metamorphic mineral facies. Pp. 407424 in: Advances in Organic Geochemistry 1%8(Schenk, P.A. & Havenaar, I., editors). Pergamon Press, Oxford.Google Scholar
Kisch, H.J. (1987) Correlation between indicators of very low-grade metamorphism. Pp. 227-300 in: Low Temperature Metamorphism(Frey, M., editor). Blackie & Son Ltd, London.Google Scholar
MacEwan, D.M.C., Ruiz Amil, A. & Brown, G. (1961) Interstratified clay minerals. Pp. 393445 in: The X-ray Identification and Crystal Structures of Clay Minerals(Brown, G., editor). Mineralogical Society, London.Google Scholar
Matsushita, H. (1949) Geology of the coal fields in Northern Kyushu. Sci. Rep. Kyushu Univ. (Geology), 3, 157 (in Japanese).Google Scholar
Mik, T. (1978) Clay mineral assemblages and Na2O-K2O contents in argillaceous rocks distributed in Amakusa, Kyushu. J. Jap. Ass. Petrol. Technologists, 43, 16–23. (in Japanese with English abstract).Google Scholar
Miki, T. (1988) Sedimentary mineralogic studies on the Tertiary sequences in Kyushu, Japan. Pp. 155166 in: Proc. Ann. Tech. Meet. Geology and Mineral Resources of Thailand (Silakul, T., editor). Chiang Mai Univ., Chiang Mai.Google Scholar
Miki, T. & Nakamuta, Y. (1985) Zeolitic diagenesis of the Paleogene formations in the Munakata coal field, Fukuoka Prefecture. J. Min. Pet. Econ. Geoi, 80, 283–291 (in Japanese with English abstract).Google Scholar
Miki, T. & Tashiro, T. (1979) Carbonaceous matter in Cretaceous-Paleogene argillaceous rocks of Amakusa, Kyushu. 29, 323330 (in Japanese with English abstract).Google Scholar
Mumpton, F.A. (1960) Clinoptilolite redefined. Atm Miner., 45, 351–369.Google Scholar
Nakamuta, Y. (1976) Zeolites and clay minerals in the Tertiary sedimentary rocks in Tsuyazaki area, Fukuoka Prefecture. J. Min. Pet. Econ. Geol., 71, 147–156 (in Japanese with English abstract).Google Scholar
Robert, P. (1985) Histoire geothermique et diagenese organique. Bull. Centr. Rech. Expl.-Prod. Elf-Aquitaine, Mem., 8, 1–345.Google Scholar
Sasaki, A., Fujioka, N. & Huzioka, K. (1982) Relation between authigenic mineral zones and maturation of organic matter in sedimentary rocks of Hokkaido, Akita and Niigata oil fields in Japan. J. Jap. Ass. Petrol. Technologists, 47, 158–167 (in Japanese with English abstract).Google Scholar
Shimoyama, T., & Iijima, A. (1977) Organic and mineral phases in burial diagenesis. Pp. 131149 in: K. Huzioka Mem. Vol. A memorial Soc. for Prof. K. Huzioka, Akita (in Japanese with English abstract).Google Scholar
Uyeda, S. & Horai, K. (1964) Terrestrial heat flow in Japan. J. Geophys. Res., 69, 2121–2141.Google Scholar
Vavra, C.L. (1989) Mineral reactions and controls on zeolite-facies alteration in sandstone of the central Transantarctic Mountains, Antarctica. J. Sed. Pet., 59, 688–703.Google Scholar