Tectonically driven dolomitization of Cambrian to Lower Ordovician carbonates of the Quruqtagh area, north-eastern flank of Tarim Basin, north-west China

Author:

Dong Shaofeng1,Chen Daizhao12,Zhou Xiqiang12,Qian Yixiong3,Tian Mi3,Qing Hairuo4

Affiliation:

1. Key Laboratory of Petroleum Resources Research; Institute of Geology and Geophysics; Chinese Academy of Sciences; No. 19, Beitucheng Xilu Chaoyang District Beijing 100029 China

2. University of Chinese Academy of Sciences; Beijing 100049 China

3. Wuxi Research Institute of Petroleum Geology; SINOPEC; Wuxi 214151 China

4. Department of Geology; University of Regina; Regina SK S4S0A2 Canada

Funder

National Key Basic Research Project

National Key Scientific Special Project

National Natural Science Foundation of China

Publisher

Wiley

Subject

Stratigraphy,Geology

Reference104 articles.

1. Stable isotope analysis of multiple carbonate samples using selective acid extraction;Al-Aasm;Chem. Geol.,1990

2. The dolomite problem: control of precipitation kinetics by temperature and saturation state;Arvidson;Am. J. Sci.,1999

3. Diagenetic fabrics of aragonite, calcite, and dolomite in an ancient peritidal-spelean environment: Triassic Calcare rosso, Lombardia, Italy;Assereto;J. Sed. Res.,1980

4. Revised equation and table for determining the freezing point depression of H2O-NaCl solutions;Bodnar;Geochim. Cosmochim. Acta,1993

5. The geometry and petrogenesis of hydrothermal dolomites at Navan, Ireland;Braithwaite;Sedimentology,1997

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