| DC Field | Value | Language |
|---|
| dc.contributor.author | Tran Nghi | - |
| dc.date.accessioned | 2020-06-25T11:12:02Z | - |
| dc.date.available | 2020-06-25T11:12:02Z | - |
| dc.date.issued | 2020 | - |
| dc.identifier.uri | http://192.168.1.231:8080/dulieusoDIGITAL_123456789/5565 | - |
| dc.description.abstract | A sccondary basin corresponds wilh a second order đepositional cycle, is limited by two erosional surfaces which arc also the boundaries of a scismic scquence. In othcr vvords, a secondary basin is a component of an overall scdimentary basin. A secondary basin is formed at the same time with a tectonic phase where the three most important factors are faulting, subsidence and uplifting. Basin-forming faults are usually normal faults and are called "syn-depositional fault" | en_US |
| dc.publisher | Đại học Quốc gia Hà Nội | en_US |
| dc.title | Method of sedimentary basin reconstruction and compilation of lithofacies - paleogeographic maps | en_US |
| Appears in Collections: | Các chuyên ngành khác
|
