Cenozoic stratigraphy and subsidence history of the South China Sea margin in the Taiwan region
Seismic reflection profiles and well data are used to determine the Cenozoic stratigraphic and tectonic development of the northern margin of the South China Sea. In the Taiwan region, this margin evolved from a Palaeogene rift to a latest Miocene-Recent foreland basin. This evolution is related to...
المؤلفون الرئيسيون: | Lin, A, Watts, A, Hesselbo, S |
---|---|
التنسيق: | Journal article |
اللغة: | English |
منشور في: |
2003
|
مواد مشابهة
-
SEISMIC STRATIGRAPHY, SUBSIDENCE HISTORY, AND TECTONIC EVOLUTION OF THE ALBORAN SEA, WESTERN MEDITERRANEAN
حسب: Watts, A, وآخرون
منشور في: (1991) -
Seismic stratigraphy and subsidence history of the united arab emirates (UAE) rifted margin and overlying foreland basins
حسب: Ali, M, وآخرون
منشور في: (2013) -
MID-CENOZOIC EVOLUTION OF SOUTH FIJI MARGINAL BASIN
حسب: Watts, A, وآخرون
منشور في: (1976) -
Subsidence history and seismic stratigraphy of the Western Musandam peninsula, Oman-United Arab Emirates Mountains
حسب: Ali, M, وآخرون
منشور في: (2017) -
Mesozoic-Cenozoic stratigraphy of the Fuegian Andes, Argentina
حسب: E.B. OLIVERO, وآخرون
منشور في: (2008-03-01)