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- W2391967355 abstract "In this paper,the depositional environment and formation mechanism of the nodular limestone from the Under Cambrian Baoshan Formation in Shidian region,western Yunnan Province was discussed on the basis of mineral components,texture and structure of the node and matrix.Researches show that there are three origins of the nodular limestone in the study area.The first is that the semi-consolidate or weak-consolidate mud and carbonate sediment is altered into the nodular structure by the differential compaction and pressure solution,and the occurrence mode of the nodular limestone is determined by the content of compositions of rock and the pressure solution intensity.The second is that the semi-consolidate or weak-consolidate mud and carbonate sediment is altered into the shoestring and rudaceous nodular limestone by the slope slumping.The third is that the argillo calcareous sediment with exposure and cracking is cemented into the nodular limestone by sediment filling." @default.
- W2391967355 created "2016-06-24" @default.
- W2391967355 creator A5043545096 @default.
- W2391967355 date "2012-01-01" @default.
- W2391967355 modified "2023-09-23" @default.
- W2391967355 title "GENESIS OF NODULAR LIMESTONE IN THE UPPER CAMBRIAN BAOSHAN FORMATION IN WESTERN YUNNAN PROVINCE" @default.
- W2391967355 hasPublicationYear "2012" @default.
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