Tectonic evolution and paleokarstification of carbonate rocks in the Paleozoic Tarim Basin

Thick carbonate rocks were developed in the depression of the Tarim craton during the Cambrian–Middle Ordovician periods. The compressional tectonic movement during the Middle Caledonian–Hercynian created the paleouplifts, which became the base for the paleokarst in the Ordovician carbonate rocks. B...

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Detalles Bibliográficos
Autores principales: Xu, Xuhui, Chen, Qianglu, Chu, Chenglin, Li, Guorong, Liu, Cunge, Shi, Zheng
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Springer Berlin Heidelberg 2016
Materias:
Original Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5674128/
https://www.ncbi.nlm.nih.gov/pubmed/29167601
http://dx.doi.org/10.1007/s13146-016-0307-4

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5674128/
https://www.ncbi.nlm.nih.gov/pubmed/29167601
http://dx.doi.org/10.1007/s13146-016-0307-4

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