Changes in source rock and reservoir properties of biosiliceous mudstone due to the migration of biogenic silica during burial diagenesis

Author:

Tsuji Takashi1,Yokoi Satoru2,Waseda Amane1,Kurokawa Shoki1,Nishita Hideki1,Okubo Susumu1,Tamagawa Tetsuya1

Affiliation:

1. JAPEX

2. JAPEX (Current affiliation: RITE)

Publisher

Japanese Association for Petroleum Engineers

Reference21 articles.

1. Abrajevitch, A., 2020: Diagenetic formation of bedded chert: Implications from a rock magnetic study of siliceous precursor sediments. Earth and Planetary Science Letters, 533, 1-11.

2. 荒木直也・加藤 進,1993:鮎川油・ガス田の発見. 石技誌,58(2),119-127.

3. Chaika, C. and Williams, L.A., 2001: Density and mineralogy variations as a function of porosity in Miocene Monterey Formation oil and gas reser voirs in California. AAPG Bulletin, 85, 149-167.

4. Goter, E. R., Picha, M. G., Sandstorm, M. A., and Schwartz, D. E., 1992: A new geological reservoir model for the Monterey: An alternativeto the "fractured shale" model. Abstract, AAPG Annual Meeting, Calary, Alberta, Canada, June 22-25.

5. Isaacs, C.M., 1981: Porosity reduction during diagenesis of the Monterey Formation, Santa Barbara coastal area, California. The Monterey Formation and Related Siliceous Rocks of California, Garrison R.E., Douglas, R.G., Pisciotto, K.E., Isaacs, C.M. and Ingle, J.C., eds., Pacific Section SEPM Special Publication, 15, 159-179.

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