Article ID Journal Published Year Pages File Type
5484128 Journal of Petroleum Science and Engineering 2017 52 Pages PDF
Abstract
The T80 unconformity in the Tarim Basin, NW China can be correlated with the Cambrian-Ordovician boundary in several other sections around the world. The detailed chemostratigraphic study and seismostratigraphic data of the Cambrian-Ordovician transition interval in the Tarim Basin are clarified. Sr element concentrations are used as a new tool for the identification and correlation of the unconformity. The lower Sr concentrations are closely correlated with the samples from the top of the Qiulitage Formation in close proximity to the T80 unconformity.192
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Economic Geology
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