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Zhu, DongYa, Jin, ZhiJun, Hu, WenXuan (2010) Hydrothermal recrystallization of the Lower Ordovician dolomite and its significance to reservoir in northern Tarim Basin. Science China Earth Sciences, 53 (3) 368-381 doi:10.1007/s11430-010-0028-9

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Reference TypeJournal (article/letter/editorial)
TitleHydrothermal recrystallization of the Lower Ordovician dolomite and its significance to reservoir in northern Tarim Basin
JournalScience China Earth Sciences
AuthorsZhu, DongYaAuthor
Jin, ZhiJunAuthor
Hu, WenXuanAuthor
Year2010 (March)Volume53
Issue3
PublisherSpringer Science and Business Media LLC
URL
DOIdoi:10.1007/s11430-010-0028-9Search in ResearchGate
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Mindat Ref. ID724301Long-form Identifiermindat:1:5:724301:5
GUID0
Full ReferenceZhu, DongYa, Jin, ZhiJun, Hu, WenXuan (2010) Hydrothermal recrystallization of the Lower Ordovician dolomite and its significance to reservoir in northern Tarim Basin. Science China Earth Sciences, 53 (3) 368-381 doi:10.1007/s11430-010-0028-9
Plain TextZhu, DongYa, Jin, ZhiJun, Hu, WenXuan (2010) Hydrothermal recrystallization of the Lower Ordovician dolomite and its significance to reservoir in northern Tarim Basin. Science China Earth Sciences, 53 (3) 368-381 doi:10.1007/s11430-010-0028-9
In(2010, March) Science China Earth Sciences Vol. 53 (3) Springer Science and Business Media LLC

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