Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
  Petroleum Geoscience   Email Content Delivery
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Petroleum Geoscience; September 2002; v. 8; no. 3; p. 279-285
© 2002 Geological Society of London
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Nansheng, Q.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Articles

Tectono-thermal evolution of the Qaidam Basin, China: evidence from Ro and apatite fission track data

Qiu Nansheng

Key Lab for Petroleum Entrapment Mechanism of Ministry of Education and Research Center for Basin & Reservoir, Petroleum University, Beijing 102249, PR China

In the Qaidam Basin, on the Northeastern Qinghai–Tibet Plateau, the thermal evolution of western and northern sub-basins was analysed using apatite fission track (AFT) data and vitrinite reflectance data from 27 wells. This study shows that thermal gradients decreased during the evolution of the basin, but there existed some differences in thermal evolution between the west and north of the basin, due to different tectonic movements. The thermal gradients in Paleocene–Miocene in the west and in Jurassic times in the north were more than 30°C km–1, exceeding present-day gradients. These thermal data can provide useful parameters for the study of the Qaidam Basin and Qinghai–Tibet Plateau. Palaeotemperature data are the critical parameter for hydrocarbon generation calculations. The results in this study provide a foundation for hydrocarbon generation history modelling and petroleum resources assessment in the Qaidam Basin.

KEYWORDS: Burial history, subsurface temperature, paleotemperature, Qaidam Basin, fission track dating, vitrinite reflectance, thermal gradient




This article has been cited by other articles:


Home page
Geological Society of America Special PapersHome page
A. Yin, Y. Dang, M. Zhang, M. W. McRivette, W. P. Burgess, and X. Chen
Cenozoic tectonic evolution of Qaidam basin and its surrounding regions (part 2): Wedge tectonics in southern Qaidam basin and the Eastern Kunlun Range
Geological Society of America Special Papers, January 1, 2007; 433(0): 369 - 390.
[Abstract] [Full Text] [PDF]


Home page
Petroleum GeoscienceHome page
Q. Nansheng, Z. Ming, W. Xulong, and Y. Haibo
Tectono-thermal evolution of the Junggar Basin, NW China: constraints from Ro and apatite fission track modelling
Petroleum Geoscience, October 1, 2005; 11(4): 361 - 372.
[Abstract] [Full Text] [PDF]




JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Geological Society of London