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来源：百度知道 编辑：UC知道 时间：2024/06/28 12:04:05
5.10 Indus Platform and Foredeep
It comprises the foot hills of Keirthar,Sulaiman ranges,the Indus Plain.Cholistan and Thar deserts. This zone is underlain by continental crust and crystalline rocks of Indian shield.The crystalline rocks are overlain by platform type shallow deposit of Mesozoic and Cenozoic age with alluvial plains making the top of the sequence.The basement rocks are extensively traversed by faults with horst and graben structures and ancient rift valleys.The sedimentary sequences are an important sources of oil,gas and coal.The up-warp zones contain deposits of Fuller's earth,dolomite,limestone and other building stones.
It comprises the foot hills of Keirthar,Sulaiman ranges,the Indus Plain.Cholistan and Thar deserts. This zone is underlain by continental crust and crystalline rocks of Indian shield.The crystalline rocks are overlain by platform type shallow deposit of Mesozoic and Cenozoic age with alluvial plains making the top of the sequence.The basement rocks are extensively traversed by faults with horst and graben structures and ancient rift valleys.The sedimentary sequences are an important sources of oil,gas and coal.The up-warp zones contain deposits of Fuller's earth,dolomite,limestone and other building stones.
梧桐平台和前渊
它包括了山上山下,苏莱曼峦、梧桐 和塔尔沙漠. 这一带是由大陆地壳和下倾印电枢结晶岩都是结晶岩平台式的复 浅金同年龄的冲积平原,新生代制作顶部基岩广泛的序列 走过了故障垒和地堑裂谷 . 沉积层序和古建筑物的重要来源,石油、天然气 煤和过硬纱区全面遏制存款的地球,白云石、石灰石、建筑石材等.
5.10 印度西北部的河流月台和 Foredeep
它包含 Keirthar 的脚小山、 Sulaiman 范围,印度西北部的河流平原。Cholistan 和 Thar 沙漠。 这地域是大陆外壳和印度盾的水晶岩石的 underlain 。水晶的岩石是月台类型的 overlain 中世代的浅存款，而且 Cenozoic 以制造序列的顶端的冲积平原变老。地下室岩石广泛地与地垒和 graben 结构和远古的裂口山谷被过失横过。沈渣的序列是一个油、瓦斯和煤的重要来源。向上-弯地域包含半圆型槌的地球、白云石的存款、石灰石和其他的建筑物石头。
5.10 Indus 平台和Foredeep 它包括脚小山Keirthar, Sulaiman 范围, Indus Plain.Cholistan 和Thar 沙漠。这个区域由大陆外壳强调并且印第安shield.The 水晶岩石水晶岩石由平台类型浅储蓄躺在上面中生并且Cenozoic 年龄与冲积平原做上面sequence.The 地下室岩石由缺点广泛地攀登与地垒和graben 结构并且古老裂口valleys.The 沉淀序列是油, 气体的重要来源并且coal.The 翘曲区域包含更加充分的地球、白云岩、石灰石和其它大厦石头储蓄
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