Discovery of the Qinghe fault, the inner part of the Weihe graben, central China, and its geological significance
The Weihe graben is an active Cenozoic continental rift with frequent seismic activity. The previous work focused on the graben boundary faults, but less work has been conducted on the faults in the internal graben. The Weihe basin is an economically developed and densely populated area. Therefore,...
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| Formatua: | Artikulua |
| Hizkuntza: | English |
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Frontiers Media S.A.
2023-04-01
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| Saila: | Frontiers in Earth Science |
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| Sarrera elektronikoa: | https://www.frontiersin.org/articles/10.3389/feart.2023.1127897/full |