Article ID Journal Published Year Pages File Type
5484536 Journal of Petroleum Science and Engineering 2017 12 Pages PDF
Abstract
Ordovician formation water may have mixed with 87Sr rich shale-derived or paleo-meteroic water (Line 1) and 87Sr rich brines up-migrated from the Lower Cambrian or Ediacaran clastic rocks (Line 2).
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Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Economic Geology
Preview
Origin and evolution of formation water from the Ordovician carbonate reservoir in the Tazhong area, Tarim Basin, NW China
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