Morphotectonic Evolution of Qaret El Sheikh Abdallah Depressions and Denuded Paleo-Karst in the White Desert, El Bahariya-Farafra Karst Territory, Egypt.

M. El-Aref, Ahmed Salama, M. Hammed
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引用次数: 2

Abstract

Corresponding author: Hammed, Mohamed Saleh Hassan, Email: salehhammed@cu.edu.eg Received 27/10/2021; Accepted 07/11/2021 DOI: 10.21608/egjg.2021.103324.1011 ©2021 National Information and Documentation Center (NIDOC) THE Late Cretaceous-Early Eocene carbonate sequences of the White Desert of Egypt exhibit amazing complex paleo-humid karst landforms, so it was declared as a nature-protected area since 2002. Two karst depressions of El Sheikh Abdallah and the Crystal Mountain (Qaret El Sheikh Abdallah) are identified by detailed fieldwork and GIS morphometric analysis of the digital elevation model of the northern part of the White Desert. These depressions are verified as two separate karst uvalas between the major karst poljes of El Bahariya and Farafra karst territory with northeast alignment. The sea-level drops and uplifting phases of the carbonate sequences of the uvalas, associated with the major compressional events of the Syrian arc (Cretaceous-Paleogene) and Oligo-Miocene extensional tectonics in north Egypt caused the development of three major stratigraphic breaks (fossilized paleo-karst surfaces) of Late Cretaceous-Palaeocene, Palaeocene-Early Eocene, and post-Early Eocene (Oligocene-Miocene). Along these fossilized surfaces, paleokarst features and sediments are detected and described. El Sheikh Abdallah and the Crystal Mountain depressions (uvalas) are also dominated by exposed (surface) complex karst features such as unroofed caves, widened joints, sinkholes, collapse breccia’s, and solution channels, together with sporadic remains of uncovered autochthonous and allochthones paleo-cave sediments. The recognized stratigraphic breaks and their paleokarst features and the subsequent surface denudation helped to propose a morphotectonic evolutionary model for the exposed karst landscape and the denuded karst features of El Sheikh Abdallah-Crystal Mountain uvalas.
埃及El Bahariya-Farafra喀斯特地区白色沙漠Qaret El Sheikh Abdallah凹陷形态构造演化与剥蚀古岩溶
通讯作者:Hammed, Mohamed Saleh Hassan, Email: salehhammed@cu.edu.eg埃及白色沙漠的晚白垩世-早始新世碳酸盐岩层序表现出令人惊叹的复杂的古湿润喀斯特地貌,因此自2002年起被宣布为自然保护区。通过详细的野外调查和对白色沙漠北部数字高程模型的GIS形态计量分析,确定了El Sheikh Abdallah和水晶山(Qaret El Sheikh Abdallah)两个岩溶洼地。这些凹陷被证实是位于El Bahariya和Farafra喀斯特地区主要喀斯特极点之间的两个独立的喀斯特乌瓦,其方向为东北方向。乌瓦拉斯碳酸盐层序的海平面下降和抬升阶段,与叙利亚弧(白垩纪-古近纪)和埃及北部渐新世-中新世伸展构造的主要挤压事件相结合,形成了晚白垩世-古新世、古新世-早始新世和后早始新世(渐新世-中新世)三个主要地层断裂(化石古岩溶面)的发育。沿着这些化石表面,可以探测和描述古岩溶特征和沉积物。El Sheikh Abdallah和水晶山洼地(uvalas)也以暴露的(表面)复杂岩溶特征为主,如无顶洞穴、加宽节理、陷落角砾岩和溶蚀通道,以及零星的未覆盖的原生和外来古洞穴沉积物遗迹。已知的地层断裂及其古岩溶特征和随后的地表剥蚀有助于为El Sheikh Abdallah-Crystal Mountain uvalas的暴露岩溶景观和剥蚀岩溶特征提出形态-构造演化模式。
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