Lithofacies Analysis and Reconstruction of Deformation Types of Cenozoic Sediments of Phú Khánh Basin

Lithofacies Analysis and Reconstruction of Deformation Types of Cenozoic Sediments of Phú Khánh Basin

From Oligocene and Quaternary geological sedimentary section have six cycles corresponding to six sequences: - Sequence 1: Eocene - early Oligocene (E2 – E 3 1 ); - Sequence 2: Late Oligocene (E3 2 ); - Sequence 3: Early Miocene (N1 1 ); - Sequence 4: Middle Miocene (N1 2 ); - Sequence 5: Late...

Full description

Saved in:
Bibliographic Details
Main Authors: Trần, Nghi, Trần, Hữu Thân, Chu, Văn Ngợi, Nguyễn, Duy Tuấn, Trần, Thị Dung, Nguyễn, Thị Phương Thảo, Phạm ThịThu Hằng, Thị Thu Hằng, Trần, Văn Sơn
Format: Article
Language:English
Published: VNU 2014
Subjects:
Sequence
lowstand
highstand
transgressive systems tract
parasequence set
parasequence
marine flooding plain
Online Access:http://repository.vnu.edu.vn/handle/11126/4631
Tags: Add Tag
No Tags, Be the first to tag this record!
Institution: Vietnam National University, Hanoi
Language: English
Description
Summary:From Oligocene and Quaternary geological sedimentary section have six cycles corresponding to six sequences: - Sequence 1: Eocene - early Oligocene (E2 – E 3 1 ); - Sequence 2: Late Oligocene (E3 2 ); - Sequence 3: Early Miocene (N1 1 ); - Sequence 4: Middle Miocene (N1 2 ); - Sequence 5: Late Miocene (N1 3 ); - 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).

Similar Items