The Carbon and Oxygen Isotope Composition of Secondary Carbonates in Volcanites of the pre-Jurassic Complex of the West Siberian Plate
- Авторлар: Krasnova A.V.1, Rostovtseva Y.V.1, Gavrilov A.E.2
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Мекемелер:
- Department of Geology, Moscow State University
- Gazpromneft STC
- Шығарылым: Том 74, № 6 (2019)
- Беттер: 567-572
- Бөлім: Article
- URL: https://journals.rcsi.science/0145-8752/article/view/175101
- DOI: https://doi.org/10.3103/S014587521906005X
- ID: 175101
Дәйексөз келтіру
Аннотация
The carbon and oxygen isotope composition of secondary carbonates from acidic effusives in the top of the pre-Jurassic complex of the West Siberian plate (Tomsk Region) was studied. The siderite values of δ13С (VPDB) and δ18О (VSMOW) vary from –6.6 to –2.4‰ and from 7.8 to 12.3‰, while the calcite values vary from –8.9 to –8.4‰ and from 2.5 to 3.7‰, respectively. The light oxygen isotope composition indicates that the carbonates were from medium- and low-temperature hydrothermal solutions.
Негізгі сөздер
Авторлар туралы
A. Krasnova
Department of Geology, Moscow State University
Хат алмасуға жауапты Автор.
Email: boxannak@gmail.com
Ресей, Moscow, 119991
Yu. Rostovtseva
Department of Geology, Moscow State University
Хат алмасуға жауапты Автор.
Email: rostovtseva@list.ru
Ресей, Moscow, 119991
A. Gavrilov
Gazpromneft STC
Хат алмасуға жауапты Автор.
Email: GavrilovAE@gaspromneft-ntc.ru
Ресей, St. Petersburg, 190000
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