NEW TYPE OF RESERVOIR IN CRYSTALLINE BASEMENT ROCK
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dc.contributor.author | Dmitriyevskiy A.N. | |
dc.contributor.author | Kireyev F.A. | |
dc.contributor.author | Bochko R.A. | |
dc.contributor.author | Fedorova T.A. | |
dc.date.accessioned | 2020-10-31T11:22:52Z | |
dc.date.available | 2020-10-31T11:22:52Z | |
dc.date.issued | 1990 | |
dc.identifier | https://elibrary.ru/item.asp?id=31093844 | |
dc.identifier.citation | Transactions (Doklady) of the USSR Academy of Sciences. Earth Science Sections, 1990, , 6, 117-119 | |
dc.identifier.issn | 0891-5571 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/18330 | |
dc.description.abstract | The shelf deposits off South Vietnam are dominated by Oligocene-to-Miocene clayey carbonate sandstones and argillites, generally resting on a silicic crystalline basement. Penetration of the basement yielded oil flows from wells in quartz-kaolinite rocks that were initially interpreted as a granite weathered crust. But additional studies using the Superprobe-733 electron microprobe, a Link Systems energy dispersion analyzer and a JSM-50A scanning electron microscope suggested a new interpretation. To summarize, our detailed analysis of the alteration of crystalline basement rocks in the shelf zone off South Vietnam has identified a fundamentally new hydrothermal type of reservoir, which will probably be increasingly encountered as deep-sea drilling in this area is expanded. | |
dc.subject | Miocene | en |
dc.subject | Oligocene | en |
dc.title | NEW TYPE OF RESERVOIR IN CRYSTALLINE BASEMENT ROCK | |
dc.type | Статья | |
dc.subject.age | Кайнозой::Неоген::Миоцен | ru |
dc.subject.age | Cenozoic::Paleogene::Oligocene | en |
dc.subject.age | Cenozoic::Neogene::Miocene | en |
dc.subject.age | Кайнозой::Палеоген::Олигоцен | ru |
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