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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...
| Autores principales: | , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Springer Berlin Heidelberg
2016
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| Materias: | |
| 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 |