对德尼兹利地区地貌构造发展的几点思考

IF 0.5 Q4 GEOSCIENCES, MULTIDISCIPLINARY Bulletin of the Mineral Research and Exploration Pub Date : 2022-07-21 DOI:10.19111/bulletinofmre.1146674

Y. Yılmaz

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引用次数: 0

摘要

代尼兹利地区位于约旦高地以东。尽管德尼兹利地区与b yy k Menderes和Gediz地堑遵循相同的趋势，但在第四纪经历了半独立的演化。该地区的基本形态构造要素是Denizli盆地及其周围的babadaku和Güzelpınar地脉。巴巴达霍斯特是该地区最独特的形态构造元素。它在北部被德尼兹利断层所包围，这是一条斜向正断层，可能是一条主要的拆离断层。老底嘉断层和Güzelpınar断层可以看作是对立的构造。

本文章由计算机程序翻译，如有差异，请以英文原文为准。

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Some thoughts on the morphotectonic development of the Denizli region Basic

The Denizli region is located to the east of the Buldan horst. Although they follow the same trends as the Büyük Menderes and Gediz grabens, the Denizli region has undergone semi-independent evolution during the Quaternary. The essential morphotectonic elements of the area are the Denizli basin and the surrounding Babadağ and the Güzelpınar horsts. The Babadağ horst is the most distinct morphotectonic element of the region. It is bounded in the North by the Denizli fault, a listric normal fault, possibly a major detachment fault. The Laodicea and Güzelpınar horsts located within the downthrown block of the fault may be regarded as antithetic structures.

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来源期刊

Bulletin of the Mineral Research and Exploration GEOSCIENCES, MULTIDISCIPLINARY-

CiteScore

1.20

自引率

20.00%

发文量

审稿时长

10 weeks

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