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《成都地质学院学报》 1987-04
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A STUDY ON DOLOMITIZATION OF TWO DEVONIAN STRATA IN THE GANXI SECTION NORTHWEST SICHUAN

Tian Hongjun Liu Xiufeng (Chengdu College of Geology)M. Schonfeld (Clausthal Techniche Universitat Deutchland)  
Carbonate rock dolomitization in Shawozi and Maoba formations of upper Devonian in Ganxi section, northwest Sichuan is studied with relevance to its sedimentary facies analysis. It is found that the sedimentary facies not only controlled types and intensity of the early dolomitization, but also influenced the subsequent stabilization of dolomite. In general, dolomite formed by replacing porous grainstone which deposited in a stiring environment is easier to become stable and ordering to compare with dolomite formed by replacing dense and clay-bearing micrite which deposited in a low environment. The CL colour of dolomite originated from freshwater replacement is rosy to light purple, Sr~(2+) content150 ppm. The CL colour of dolomite formed by sea water replacement is yellow, Sr~(2+) Content150 ppm. Calcite cement of fresh water origin has no luminescence, or dark brown CL. Seawater calcite cement has orange CL.Two dolomitization models are established.
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