PALEOMAGNETISM OF DYKES AND TUFFS FROM THE MESUDIYE REGION AND ROTATION OF TURKEY

被引：34

作者：

ORBAY, N ^{[1
]}

BAYBURDI, A ^{[1
]}

机构：

[1] UNIV NEWCASTLE UPON TYNE,SCH PHYS,NEWCASTLE TYNE NE1 7RU,TYNE & WEAR,ENGLAND

来源：

GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY | 1979年 / 59卷 / 03期

关键词：

D O I：

10.1111/j.1365-246X.1979.tb02565.x

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

Summary. The pole positions obtained from Upper Cretaceous and Eocene tuffs and dykes of the Mesudiye region, which is located between the north of the North Anatolian Fault Zone and eastern Black Sea coast, are at 75.3° N, 275.4° E and 41.7° N, 138.6° E respectively. These results, taken together with the results of previous studies of Turkish rocks, suggest that rotational movements of Turkey have been 45–50° counterclockwise to Europe since the Upper Cretaceous. Copyright © 1979, Wiley Blackwell. All rights reserved

引用

页码：437 / 444

页数：8

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