基于形态构造和构造资料的北安纳托利亚断裂带南支乌鲁巴特湖南部和苏苏鲁克河谷活动断裂模式——对安纳托利亚西北部弯曲模式的批判

IF 1.3 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Turkish Journal of Earth Sciences Pub Date : 2022-01-01 DOI:10.55730/1300-0985.1759
G. Seyitoğlu, Korhan Esat
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引用次数: 2

摘要

乌鲁巴特湖以南和苏苏鲁克山谷的野外观测和形态构造评价表明,主要的活动断裂样式由东北-西南和东北-西-西南右侧断层以及在这些走滑断层之间发育的西北-东南正断层组成。我们重新定义了乌鲁巴特湖以南的活动断层,发现这些东北-西南的右侧断层控制着苏苏鲁克河的路线。根据这些发现和评估,我们可以声称之前为该地区提出的“弯曲模型”是无效的,如Mustafakerpaşa断层和Balıkesir-Kepsut断层的例子所示。相反,我们建议属于北安那托利亚断层带南部分支的断层通过布尔萨、苏苏鲁克和巴尔凯希尔延伸至阿赫萨尔和伊兹密尔。
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The active fault pattern based on morphotectonic and structural data in the south ofUlubat Lake and the Susurluk valley along the southern branch of North Anatolian FaultZone: A criticism of the bend model in northwest Anatolia
: Field observations and morphotectonic evaluations on the south of Ulubat Lake and the Susurluk valley show that the dominant active fault pattern consists of northeast-southwest and east northeast-west southwest right-lateral faults and northwest-southeast normal faults developing between these strike-slip faults. We redefined the active faults in the south of Ulubat Lake and discovered that these northeast-southwest right-lateral faults control the route of Susurluk River. Based on these discoveries and evaluations, we can claim that the “bend model” previously proposed for the region is not valid, as seen in the Mustafakemalpaşa Fault and Balıkesir-Kepsut Fault examples. Instead, we suggest that the faults belonging to the southern branch of the North Anatolian Fault Zone extend to Akhisar and İzmir via Bursa, Susurluk, and Balıkesir.
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来源期刊
Turkish Journal of Earth Sciences
Turkish Journal of Earth Sciences 地学-地球科学综合
CiteScore
2.40
自引率
10.00%
发文量
6
审稿时长
6 months
期刊介绍: The Turkish Journal of Earth Sciences is published electronically 6 times a year by the Scientific and Technological Research Council of Turkey (TÜBİTAK). It is an international English-language journal for the publication of significant original recent research in a wide spectrum of topics in the earth sciences, such as geology, structural geology, tectonics, sedimentology, geochemistry, geochronology, paleontology, igneous and metamorphic petrology, mineralogy, biostratigraphy, geophysics, geomorphology, paleoecology and oceanography, and mineral deposits. Contribution is open to researchers of all nationalities.
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