Abstract
Based on the strata, lithologic association and coal-bearing property – using the method of synthetic correlation – the relation between limestone layers and the thick coal seam of the Taiyuan Form...
Highlights
Late Paleozoic coal-bearing series research of Shanxi province began in the 18th century
In the perspective of lithofacies palaeogeography and sequence stratigraphy, a chaos subdivision of multiple can be divided into several points: proposed the boundary at the eighth coal seam in the Taiyuan area, which corresponds a larger relative fall of the sea level, and Miaogou limestone, as its top surface of the eighth coal seam is located in the Permian strata (Li et al, 1999); proposed the boundary during in the bottom of Miaogou limestone, the ninth coal seam and bauxitic mudstone (Shao et al, 2014); proposed in the bottom of the ninth coal seam (Lu et al, 2012); and lined Maoergou limestone (Li et al, 2006)
Based on the analysis of the coal seam and limestone of Taiyuan Formation in Shanxi province, we conclude with the following statements
Summary
Late Paleozoic coal-bearing series research of Shanxi province began in the 18th century. In the Datong – Huairen area, the thickness of the strata ranges from 75 to 115 m up to 115 m, and decreases from north to south without marine limestone development.
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