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Geologic and economic potentials of minerals and industrial rocks in Jordan

机译：约旦的矿物和工业岩石的地质和经济潜力

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This work discusses status of the geologic and economic potentials of minerals and industrial rocks in Jordan. The major mineral resources are presented in details and the paper is designed to cover the lack of published data in this field. Geologically, the structural framework of Jordan is controlled largely by Arabian Nubian Shield in the south, block—faulted areas in the east, upwarping in north and east, and Wadi Araba-Dead Sea Transform Fault in the western part. The geologic environments include Precambrian crystalline basement (Late Proterozoic) of Arabian Nubian Shield (ANS) that is composed of igneous and metamorphic rocks at south-western part. Paleozoic rocks at southern and southeastern part consist of clastic minerals which are dominated by sandstone, whereas Mesozoic sedimentary rocks are widespread throughout southwestern, northern to southeastern parts of the country. They mainly consist of major industrial rocks and minerals such as phosphate, oil shale, limestone, dolomite, chalk, marble, gypsum, diatomite and tripoli. Cenozoic Era is composed of sedimentary and volcanic rocks in different parts of Jordan. There are more than twenty nonmetallic minerals and four main metallic deposits within the various geologic environments. This paper summarizes their distribution, chemical and mineralogical characteristics, in addition to their production statistics.
机译：这项工作讨论了约旦矿产和工业岩石的地质和经济潜力状况。详细介绍了主要矿产资源，本文旨在弥补该领域缺乏公开数据的问题。在地质上，约旦的结构框架主要由南部的阿拉伯努比亚盾构，东部的块状断裂区域，北部和东部的翘曲区域以及西部的Wadi Araba-Dead Sea转换断层控制。地质环境包括阿拉伯努比亚盾（ANS）的前寒武纪晶体基底（晚期元古代），该基底由西南部的火成岩和变质岩组成。南部和东南部的古生代岩石由碎屑矿物组成，以砂岩为主，而中生代沉积岩遍布该国的西南，北部至东南部。它们主要由主要的工业岩石和矿物组成，例如磷酸盐，油页岩，石灰石，白云石，白垩，大理石，石膏，硅藻土和三叶草。新生代时代由约旦不同地区的沉积岩和火山岩组成。在各种地质环境中，有二十多种非金属矿物和四个主要金属矿床。除了生产统计数据外，本文还概述了它们的分布，化学和矿物学特征。

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