DC Field | Value | Language |
dc.contributor.author | Trần Nghi | - |
dc.date.accessioned | 2020-06-25T22:45:54Z | - |
dc.date.available | 2020-06-25T22:45:54Z | - |
dc.date.issued | 2020 | - |
dc.identifier.uri | http://192.168.1.231:8080/dulieusoDIGITAL_123456789/6146 | - |
dc.description.abstract | From Oligocene and Quaternary geological sedimentary section have six cycles corresponding to six sequences: - Sequence 1: Eocene - early Oligocene (E2 – E31); - Sequence 2: Late Oligocene (E32); - Sequence 3: Early Miocene (N11); - Sequence 4: Middle Miocene (N12); - Sequence 5: Late Miocene (N13); - Sequence 6: Pliocene - Quaternary (N2 - Q). Since then may establish three general integrated formulas between the lithofacies association series and sedimentary systems tract as follows: 1. Sedimentary lowstand systems tract (LST): LST = arLST + (ar + amr)LST + (amt + mt)/(amr + mr) LST + mrLST (1); 2. Sedimentary transgressive systems tract (TST): TST = MtTST + atTST + (amr + mr)/(mt + amt)TST + mtTST (2); 3. Sedimentary highstand systems tract (HST): HST = arHST + (ar + amr)HST + (amt+mt)/ (amr + mr)HST + mrHST (3). | en_US |
dc.publisher | Đại học Quốc gia Hà Nội | en_US |
dc.title | Lithofacies Analysis and Reconstruction of Deformation Types of Cenozoic Sediments of Phú Khánh Basi | en_US |
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