| Tectonic Factors Favourable for the Formation of Evaporites in the Indosinian Period in Hubei and Its Neighbouring Areas |
| |
| 摘 要： | 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.
|
Tectonic Factors Favourable for the Formation of Evaporites in the Indosinian Period in Hubei and Its Neighbouring Areas |
| |
| Authors: | Li Shiruo |
| |
| Abstract: | Abstract In the Indosinian period, the climate was scorching hot and the source of seawater was ample in Hubei and its neighbouring 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 between the Jiangnan oldland-upwarped zone and the Dabashan upwarped zone differ in degree of development is mainly due to the tectonic factors during sedimentation. If favourable tectonic factors are present, large amounts of evaporites will form; on the contrary, they will not. |
| |
| Keywords: | |
| 本文献已被 CNKI 等数据库收录！ |
| 点击此处可从《Acta Geologica Sinica》浏览原始摘要信息 |
| 点击此处可从《Acta Geologica Sinica》下载免费的PDF全文 |
