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《成都地质学院学报》 1988-01
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THE CATHODOLUMINESCENCE AND DIAGENESIS OF THE CARBONATES OF GUANWUSHAN FORMATION, MIDDLE DEVONIAN, GANXI, NORTHWESTERN SICHUAN

Huang Sijing  
Cathodoluminescent pheatures of the carbonates of the Guanwushan Forma-tion (D_2), Ganxi, NW Sichuan are studied. According to the principle thatcathodoluminescent intensity is mainly controlled by Fe~2 concentration andtaking in consideration of other analytical data and field observation,dolomitization, cementation and neomorphism processes are investigated. Thesequences of diagenesis of the Guanwushan carbonates are established.
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【Co-references】
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【Secondary References】
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