Thermal maturity of Carboniferous to Eocene Sediments of the Alpine-Dinaric Transition Zone (Slovenia)
详细信息 查看全文
- 作者：T. Rainera ; 1 ; thomas.rainer@omv.com" class="auth_mail" title="E-mail the corresponding author ; R.F. Sachsenhofera ; reinhard.sachsenhofer@unileoben.ac.at" class="auth_mail" title="E-mail the corresponding author ; P.F. Greenb ; G. Rantitscha ; gerd.rantitsch@unileoben.ac.at" class="auth_mail" title="E-mail the corresponding author ; U. Herlecc ; uros_herlec@yahoo.co.uk" class="auth_mail" title="E-mail the corresponding author ; M. Vrabecc ; marko.vrabec@ntf.uni-lj.si" class="auth_mail" title="E-mail the corresponding author
- 关键词：Vitrinite reflectance ; Flysch ; Slovenian Basin ; Southern Alps ; Northern Dinarides
- 刊名：International Journal of Coal Geology
- 出版年：2016
- 出版时间：1 March 2016
- 年：2016
- 卷：157
- 期：Complete
- 页码：19-38
- 全文大小：5815 K
文摘
- •
Maturity of Mesozoic rocks in the Alpine-Dinaric transition zone is controlled by thickness of Cretaceous to Paleogene rocks.
- •
Highest maturity is observed in the Slovenian Basin.
- •
High vitrinite reflectance in Cretaceous sediments (up to 4.4 %Rr) is due to very thick Paleogene flysch sediments.
- •
Uplift and cooling occurred between Late Eocene and Mid Oligocene time.
- •
Thrusting postdates maturation.