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PROSPECTIVE PETROLIFEROUS AREAS IN THE EAST CHINA SEA BASIN

PROSPECTIVE PETROLIFEROUS AREAS IN THE EAST CHINA SEA BASIN The East China Sea Basin is a major Cenozoic basin, with a sedimentary fill greater than 10,000 metres in thickness. The evolution of the basin is divisible into four stages‐down‐faulting, fault‐sagging, down‐warping and draping. Tectonic movements were characterized by multiple episodes of spatial differentiation, and tectonic units are divisible into longitudinal zones and latitudinal blocks. Various types of trap structure are present, including Tertiary sandstone traps, basement traps, and reef traps. http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Journal of Petroleum Geology Wiley

PROSPECTIVE PETROLIFEROUS AREAS IN THE EAST CHINA SEA BASIN

Journal of Petroleum Geology , Volume 13 (1) – Jan 1, 1990

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References (3)

Publisher
Wiley
Copyright
Copyright © 1990 Wiley Subscription Services
ISSN
0141-6421
eISSN
1747-5457
DOI
10.1111/j.1747-5457.1990.tb00252.x
Publisher site
See Article on Publisher Site

Abstract

The East China Sea Basin is a major Cenozoic basin, with a sedimentary fill greater than 10,000 metres in thickness. The evolution of the basin is divisible into four stages‐down‐faulting, fault‐sagging, down‐warping and draping. Tectonic movements were characterized by multiple episodes of spatial differentiation, and tectonic units are divisible into longitudinal zones and latitudinal blocks. Various types of trap structure are present, including Tertiary sandstone traps, basement traps, and reef traps.

Journal

Journal of Petroleum GeologyWiley

Published: Jan 1, 1990

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