使用形态计量指数确定土耳其马尔马里斯Bozburun半岛构造与岩溶作用之间的关系

IF 0.5 Q4 GEOSCIENCES, MULTIDISCIPLINARY Bulletin of the Mineral Research and Exploration Pub Date : 2023-07-19 DOI:10.19111/bulletinofmre.1329619
İsmail Ege, Efekan Özkan, Selahattin Polat
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引用次数: 0

摘要

Bozburun半岛(Marmaris)因其在不同时期的石灰岩上具有不同的岩溶形状而备受关注,也是一个重要的构造活动区域。本研究考察了由卫星图像、地形图和实地研究确定的岩溶形状的面积大小,它们聚集的海拔、坡度、深度值范围和扩展,并确定了影响它们的断层线。为了定量解释这一效应,采用了形态计量学形状指标中的伸长率(RE)和伸长率方向(EA α)。另一方面,Poljes与dolines和uvalas分开进行了更详细的评估,计算了点蚀率(PR)。通过遥感(RS)、地理信息系统(GIS)技术和野外观测相结合的研究,认为古构造和新构造时期西部金牛座岩溶地区的褶皱和裂缝对岩溶作用有积极作用,并确定了岩溶形态的走向与断裂的走向有很大的相似性。
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Determination of the relationship between tectonic and karstification using morphometric indices in Bozburun Peninsula, Marmaris, Türkiye
Bozburun Peninsula (Marmaris) attracts attention because it contains various karstic shapes on limestones belonging to different periods and it is also an important area in terms of tectonic activity. This study examines the area sizes of the karstic shapes determined by satellite images, topographic maps and field studies, the elevations, slopes, depth value ranges and extensions where they are clustered and the fault lines affecting them have been determined. In order to explain this effect quantitatively, the elongation ratio (RE) and elongation direction (EA α) from morphometric shape indices were used. Poljes, on the other hand, were evaluated in more detail separately from dolines and uvalas, the pitting rates (PR) was calculated. It was understood that in this study which Remote Sensing (RS), Geographic Information System (GIS) technologies and field observations were correlated, folds and fractures that occurred in the Western Taurus Karst Region during the paleotectonic and neotectonic periods had a positive effect on karstification, and it was determined the lie of the karstic shapes to a great extent resemblance to the lie of the faults.
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来源期刊
Bulletin of the Mineral Research and Exploration
Bulletin of the Mineral Research and Exploration GEOSCIENCES, MULTIDISCIPLINARY-
CiteScore
1.20
自引率
20.00%
发文量
22
审稿时长
10 weeks
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