fault basin造句

• The chezhen depression as a fault basin is located in the northeastern part of the bohaiwan basin in shandong
  摘要车镇凹陷古近系沙河街组三段上亚段二段下亚段是较为典型的深断陷型三级层序。
• Santanghu basin is a congruent & reconstruct innertief , which developed on the basis of rift - fault basin of permian
  三塘湖盆地是一个在二叠纪裂谷-断陷盆地基础上发展起来的叠合、改造型山间盆地。
• Hegang coal field , of the type of a ( inland ) faulted basin far from the sea , was formed in the early neo - jurassic age about 140 million years ago
  鹤岗煤田约形成于一亿四千多万年前的晚侏罗世初期，是远海内陆断陷盆地型煤田。
• Lying in the east of heilongjiang province , yishu graben is a cenozoic fault basin comprising two large second - class structural units , i . e . , tangyuan and fangzheng fault basins
  摘要依舒地堑位于黑龙江省东部，为新生代断陷盆地，汤原断陷和方正断陷为其两个面积较大的二级构造单元。
• The sedimentary geochemistry analysis indicates that the middle and lower yangtze basin is the craton basin , and shangrao and mingxi basins are the continental margin fault basins in the early triassic
  早三叠世的中下扬子混积盆地属克拉通边缘盆地，而上饶和明溪碎屑岩盆地则为大陆边缘断陷盆地。
• Niuxintuo area in liaohe depression is a fault basin , tectonic movement is complex and fault is developed at the basement and at the late stage , where the conditions for creating various hydrocarbon reservoirs are provided
  摘要辽河坳陷牛心坨地区为断陷湖盆，基底及后期的构造活动复杂，断层发育，具有形成各类隐蔽油气藏的地质条件。
• In the present survey and valuation the area is divided into three parts : exposed karst region in upwarped distric , karst region controlled by folded structures near depressed belts and blinded karst region in fault basins
  目前开展的可有效利用的地下水资源调查评价将该区划分为隆起带裸露岩溶分布区、沉降带边缘褶皱构造控制岩溶分布区和断陷盆地隐伏岩溶分布区。
• The fault at the east boundary of tangyuan fault basin is a basin - controlling fault , and the faults at both the east and the west boundaries of fangzheng fault basin are also a basin - controlling fault , with the west boundary fault at fangzheng being the major one
  断层的生长指数分析表明，依舒地堑内部的北西向断裂与边界断裂的活动具有一致的规律性，都起到协调边界断裂演化发展的作用。
• According to granite ages cutting ruptures , mineralized quartz veins ages corresponding to fold deformation and formation ages of bilateral faulted basin , deformation age are limited , that are 100 ~ 65ma for one and form 65ma to the present for two and three
  根据断裂截切的花岗岩体年龄、同期褶皱变形的含矿石英脉年龄以及断裂两侧断陷盆地的形成时代，大致限定第1期变形时代为100 65ma ，第2 、 3期变形时代为65ma现今。
• Compared with lehua manganese deposit in pingxiang - leping faulted basin , which is a sedimentary hydrothermal superimposed type , both orebodies are different obviously in orebody scale , ore type and tenor of manganese etc . , it should be a deposit with different genetic type
  并与萍一乐断陷盆地内的沉积加热液叠改型乐华锰矿床进行了对比分析，二者在矿体规模、矿石类型、锰品位等方面存在显著差别，应属不同成因类型的矿床。
• The environment is favorable for the formation oil and gas ; ( 4 ) although the sedimentary environment in the two basins is cardinally identical , the evolution and difference in climate and sedimentary environemt decided the divergence of biotic characters in the two fault basins , and then the biota controlled the type and quality of fossil fuel
  尽管两大盆地在沉积环境的演化上大体一致，但气候和沉积环境的演变和差异决定了两大断陷盆地生物面貌上的差异，从而直接控制了化石燃料形成的类型和质量。
• Some conclusions are listed as follows : the plateform cover cap of ordos basin and its circumference areas can be divided into five tectonic sequences . the tectonic evolution of ordos basin can be classified in six stages : the basement formation phase ( from archeozoic to paleoproterozoic ) ; the aulacogen phase ( from mesoproterozoic to neoproterozoic ) ; the north china continental sea phase ( from sinian to early - paleozoic ) ; the north china intracratonic depression phase ( from late - paleozoic to early mesozoic ) ; large ordos inland basin phase and the formation of independent ordos basin ( mid - late mesozoic ) ; fault basin phase around the ordos basin ( cenozoic )
  通过研究有以下成果及认识：鄂尔多斯盆地及其周缘地区沉积盖层可划分为五大构造层序，盆地的形成和演化分为六大构造阶段：太古代至古元古代基底形成阶段、中新元古代克拉通内裂陷槽或坳拉槽演化阶段、震旦纪?早古生代华北陆表海盆演化阶段、晚古生代?早中生代华北克拉通坳陷演化阶段、中生代中晚期大鄂尔多斯内陆盆地演化阶段及独立鄂尔多斯盆地的形成、新生代周缘断陷盆地演化阶段。