Polyphase deformation features and extensional detachment faults on the northern and southern edges of the Nigde Massif (Central Anatolia-Turkey)

IF 2 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY
Ramazan Demircioğlu
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引用次数: 0

Abstract

The polyphase deformation features and detachment faults on the northern (Gumusler) and southern (Camardı) borders of the Nigde Massif rocks, as well as the structures developed as a result of these faults, are investigated in this paper. The Nigde Massif in the studied areas is basement Palaeozoic–Mesozoic metamorphic units. The Late Cretaceous Uckapılı granodiorite and Sineksizyayla meta-gabbro introduced the Nigde massif. These units are overlain unconformably by Late Cretaceous-Quaternary rocks. The metamorphic rocks on the massif's southern edge underwent 5-phase ductile deformation, whereas the metamorphic rocks on the northern margin underwent 3-phase folding. Both the northern and southern edges include post-Middle Eocene extensional detachment features. These are most likely extensional detachment faults related to the massif's uplift. Central Anatolia is still under an extensional tectonic regime today. Therefore, detachment fault activity and occurrence continue. A large portion of the low-angle normal faults shows an extensional detachment feature. The detachment faults identified north and south of the study area are also active today.

Abstract Image

尼格代地块(土耳其安纳托利亚中部)南北边缘的多相变形特征和伸展剥离断层
本文研究了尼格代地块岩石北部(古穆斯勒)和南部(卡马迪)边界的多相变形特征和剥离断层,以及这些断层所形成的构造。所研究地区的尼格代山丘为古生代-中生代变质岩基底。白垩纪晚期的 Uckapılı 花岗闪长岩和 Sineksizyayla 元辉长岩引入了尼格代地块。这些单元被晚白垩世-第四纪岩石不整合地覆盖。地块南缘的变质岩经历了五期韧性变形,而北缘的变质岩则经历了三期褶皱。北部和南部边缘都有中新世后的延伸剥离特征。这些很可能是与地块隆起有关的伸展剥离断层。如今,安纳托利亚中部仍处于伸展构造体系之下。因此,剥离断层的活动和出现仍在继续。低角度正断层的很大一部分都显示出伸展剥离特征。在研究区域北部和南部发现的剥离断层如今也很活跃。
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来源期刊
Solid Earth Sciences
Solid Earth Sciences GEOSCIENCES, MULTIDISCIPLINARY-
CiteScore
3.60
自引率
5.00%
发文量
20
审稿时长
103 days
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