COMPARISON OF LITHOLOGIC MAPPING WITH ASTER AND HYPERION DATA: A CASE STUDY IN THE NORTHERN OF ZARA (SİVAS), TURKEY

Oktay Canbaz, R. Atun, Önder Gürsoy, A. Gökce, T. Türk, A. C. Birdal
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引用次数: 1

Abstract

Hydrothermal alteration is one of the most important steps in the exploration of precious ore deposits. In this study, it is aimed to detect the hydrothermal alteration areas and mineral contents they preserve with ASTER and Hyperion satellite images and compare the obtained results. Because of the presence of intensive hydrothermal alteration and poor vegetation, the area which is located at the northern part of Zara district of Sivas Province has been chosen as the study area. Contact zones of Argillic (Kaolinite, illite), phyllic (serisite, muscovite) and propylitic (chlorite, calsite, epidote) alteration areas were detected with field studies, petrographic and geochemical investigations. The spectral signatures of hydrothermal minerals were measured via ASD spectroradiometer from the representative samples belonging to hydrothermal alteration study areas. According to the results, obtaining the hydrothermal alteration maps from ASTER and Hyperion satellite data are in coincide with the geological map.
岩性填图与aster和hyperion数据的比较:以土耳其zara北部(sİvas)为例
热液蚀变是寻找珍贵矿床的重要步骤之一。本研究的目的是利用ASTER和Hyperion卫星图像检测热液蚀变区及其保存的矿物含量,并对所得结果进行比较。由于存在强烈的热液蚀变,植被较差,因此选择位于Sivas省Zara地区北部的区域作为研究区。通过野外考察、岩石学和地球化学调查,发现了泥质(高岭石、伊利石)、绿质(绢云母、白云母)和丙质(绿泥石、方解石、绿帘石)蚀变区的接触带。利用ASD光谱辐射计对热液蚀变研究区代表性样品的热液矿物光谱特征进行了测量。结果表明,利用ASTER和Hyperion卫星资料获得的热液蚀变图与地质图吻合较好。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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