【摘 要】
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In the Indosinian period. the climate was scorching hot and the source of seawater was ample in Hubeiand its neighbouring areas. so the basic conditions for th
【出 处】
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Acta Geologica Sinica(English Edition)
论文部分内容阅读
In the Indosinian period. the climate was scorching hot and the source of seawater was ample in Hubeiand its neighbouring areas. so the basic conditions for the formation of evaporites were favourable. Under thisprerequisite. the reason why salt deposits occurring in some third-order tectonic units between the Jiangnanoldland-upwarped zone and the Dabashan upwarped zone differ in degree of development is mainly due to thetectonic factors during sedimentation. If favourable tectonic factors are present, large amounts or evaporiteswill form: on the contrary. they will not.
The the climate was scorching hot and the source of seawater was ample in Hubeiand its neighboring areas. So the basic conditions for the formation of evaporites were favourable. Under this prerequisite. The reason why salt deposits occurring in some third-order tectonic units favor the tectonic factors during presentations, large amounts or evaporiteswill form: on the contrary. they will not.
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