Carbon and oxygen isotope variation and its implication for marine sequence: A case study of Ordovician in Tarim Basin
Carbon and oxygen isotopes of marine carbonate rocks or fossil shells could indicate global sea-level relative change. Generally, heavier carbon isotopes or lighter oxygen isotopes reflected rise of global sea-level relative changes, and vice versa. For carbonate rocks deposited before Tertiary, car...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
KeAi Communications Co., Ltd.
2017-09-01
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| Series: | Petroleum Research |
| Online Access: | http://www.sciencedirect.com/science/article/pii/S209624951730087X |