An intensive geological survey and study on the lateral section prove that the the Tangshang Formation in different basins of eastern Zhejiang is not of the same horizon.
详细的地质调查和剖面研究,证实了浙东不同盆地原划分的塘上组并非都为同一层位。
An intensive geological survey and study on the lateral section prove that the the Tangshang Formation in different basins of eastern Zhejiang is not of the same horizon.
详细的地质调查和剖面研究,证实了浙东不同盆地原划分的塘上组并非都为同一层位。
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