STRATIGRAPHY AND PALEOGEOGRAPHY OF THE NORTHERN MARGIN OF THE ARABIAN PLATFORM DURING MESOZOIC (SOUTHEASTERN TURKEY)

被引：0
|
作者：
FOURCADE, E
DERCOURT, J
GUNAY, Y
AZEMA, J
KOZLU, H
BELLIER, JP
CORDEY, F
CROS, P
DEWEVER, P
ENAY, R
HERNANDEZ, J
LAUER, JP
VRIELYNCK, B
机构：
[1] TPAO ARAMA GRUBU,ANKARA,TURKEY
[2] UNIV PARIS 06,GEOTECHTON LAB,F-75252 PARIS,FRANCE
[3] UNIV LYON 1,DEPT SCI TERRE,CNRS,URA 11,F-69622 VILLEURBANNE,FRANCE
[4] UNIV PARIS 06,PETROL MINERAL LAB,CNRS,URA 0738,F-75252 PARIS,FRANCE
[5] INST PHYSION GEN,STRASBOURG,FRANCE
来源：
BULLETIN DE LA SOCIETE GEOLOGIQUE DE FRANCE | 1991年 / 162卷 / 01期
关键词：
THOLEIITIC BASALT; KOCALI; MESOZOIC; OPHIOLITES; PALEOGEOGRAPHY; RADIOLARITES; TETHYS; SE TURKEY;
D O I：
暂无
中图分类号：
P [天文学、地球科学];
学科分类号：
07 ;
摘要：
In southeastern Turkey, the distal margin of the Arabian platform is overthrust by the Hezan allochthonous units consisting of Liassic sediments of inner carbonate platform origin and of thin Bathonian to Maastrichtian deep-water deposits. The pelagic sequence is interrupted by numerous hiatuses and punctuated by intercalated turbidites. These stable margin units are overthrust by ophiolites. Triassic tholeiitic pillow lavas of MORB type discovered for the first time in southeastern Turkey, and by Triassic to Hauterivian radiolarites belonging to the Kocali Unit. These radiolarites are derived from a Mesozoic through bordered to the south by the Arabian platform. The Kocali Unit documents the longevity of radiolarite deposition in this art of the Tethys.
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页码：27 / 41
页数：15
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