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ASTER mapping of limestone formations and study of caves, springs and depressions in parts of Sultanate of Oman

机译:阿曼苏丹国部分地区石灰石地层的ASTER制图和洞穴,泉水和洼地的研究

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Caves, springs, and large depressions of limestone karst formations are becoming more attractive tourist places and have potential importance on socio-economic development. The present study is a multi-scale point of view on limestone karst, from the space images to microscopic fabric. Here, the karst features consist of limestone formations of Cretaceous (Albian-Cenomanian) age of Tanuf Valley and Tertiary (Late Paleocene-Middle Eocene) age of Sur region of parts of Sultanate of Oman which are mapped in the visible near-infrared and shortwave infrared spectral bands of advanced spaceborne thermal emission and reflection radiometer (ASTER) using decorrelated stretch image processing technique and the occurrences of caves, springs, and depressions of the formations in the field were studied. The decorrelated RGB images of ASTER spectral bands 8, 3, and 1 discriminated well the limestone formations and associated lithology. The limestone formations of Tanuf valley (Natih formations of Hajar unit) are thick-bedded, massive, shallow marine limestone and clayey limestone, which have caves and springs. Large depressions are studied as collapsed structures at the boundary between Abat formations; they consist of gray to white marly or micritic limestone with chert nodules and Seeb Formation of bioclastic limestone, cal-carenite, marl, and sandstone of Sur region. Interpretations of limestone formations, their occurrences and distributions of caves, springs and depressions of these regions are verified and confirmed in the field and studied in the laboratory. Occurrences of more springs and depressions in the limestone formations of the study sites are interpreted and located on the Google Earth image. The study proved the capability of ASTER sensor in mapping of limestone formations and recommends the technique to other geographical regions where similar geological questions need to be resolved.
机译:石灰岩喀斯特地貌的洞穴,泉水和大洼地正变得越来越吸引游客,并且对社会经济发展具有潜在的重要性。从空间图像到微观织物,本研究是对石灰岩喀斯特地貌的多尺度观点。在这里,喀斯特地貌特征由塔努夫河谷的白垩纪(阿尔比-新生代)时代的石灰岩地层和阿曼苏丹国部分地区的苏尔地区的第三纪(晚古新世-中始新世)时期的石灰岩形成,它们被映射在可见的近红外和短波中研究了采用去相关拉伸图像处理技术的先进星载热发射和反射辐射计(ASTER)的红外光谱带,并研究了野外洞穴,泉水和凹陷的发生。 ASTER光谱带8、3和1的去相关RGB图像很好地区分了石灰岩地层和相关的岩性。塔努夫河谷的石灰岩地层(哈贾尔单元的纳提赫地层)为厚层,块状,浅海相石灰岩和粘土质石灰石,具有洞穴和泉水。大型凹陷被视为阿巴特编队之间边界处的坍塌结构。它们由灰白色至灰白色的灰白色或微粉红色的石灰岩和硅酸盐结节以及苏尔地区的生物碎屑石灰岩,钙钙长岩,泥灰岩和砂岩的塞布形成组成。在这些领域中对石灰岩地层的解释,它们在这些地区的洞穴,泉水和洼地的发生和分布进行了验证和确认,并在实验室中进行了研究。研究地点的石灰岩地层中更多的泉水和洼地的发生被解释并位于Google Earth图像上。这项研究证明了ASTER传感器在石灰岩地层测绘中的能力,并将该技术推荐给需要解决类似地质问题的其他地理区域。

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