• 而强烈的顺层岩溶作用和构造应力引发的破裂作用是轮古东地区奥陶系碳酸盐岩岩溶型储层发育的主控因素。

    And the strong karstification in the same direction as layer and cataclasis create by tectonic stress are the control factors of Ordovician carbonate karst reservoir development.

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  • 西负苍山,东眺碧海,南北分别与佛顶、古陌岭群峰相望。

    Backed Cangshan to the west, facing sea to the east, and Foding, Gumoling to the north and south respectively.

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  • 这是历年来对该地进行的首次主动发掘,为关中西部和古“豳”地东缘地带先周时期遗存研究提供了一批重要的考古资料。

    This excavation of the site has provided a number of important archaeology materials for research on remains of Pre-Zhou Dynasty.

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  • 康古尔金矿床位于东天山康古尔·塔格韧性剪切带的南缘过渡带,矿床受脆-韧性剪切带控制。

    The Kanggul gold deposit is situated in the southern margin of the Kanggultage ductile shear zone and controlled by the brittle ductile shear belt.

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  • 东天山康古尔·塔格金铜矿带位于塔里木板块东北部晚古生代阿齐山—雅满苏火山弧岛带的北缘。

    The Kanggultage gold-copper ore belt is located in the northern late Paleozoic Aqishan - Yamansu island arc belt in the northeast of Tarim plate.

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  • 通过对区域应力场、古地貌和断裂空间展布等分析,认为垦东地区发育“隐伏型”走滑断裂。

    Through the analysis on stress field, palaeogeomorphology and spatial distribution of faults, Kendong region is considered to be 'concealed' strike - slip fault.

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  • 古近系原始地层厚度分布反映出东濮凹陷在古近纪具有裂陷盆地的构造古地理特点,但是古近纪不同时期裂陷盆地的特征有明显的差异。

    The distribution of original stratigraphic thicknesses shows that the Dongpu Sag was a rifted basin in the Paleogene, while the characteristics of different periods were obviously different.

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  • 加里东中期奥陶系碳酸盐岩古岩溶储层作为未来塔河油田重要的勘探领域,有助于今后该油田的油气勘探。

    Since the middle Caledonian karst reservoir is an important region for future exploration in the Tahe oilfield, it is believed to be a great help for petroleum exploration.

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  • 南堡凹陷南堡2号构造带主要含油层段为古近系东营组东一段砂岩及奥陶系灰岩。

    The main oil-bearing horizons of the No. 2 structural belt of the Nanpu subbasin are sandstone of the First Member of the Paleogene Dongying Formation and Ordovician limestone.

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  • 鄂尔多斯盆地南部加里东期风化壳储集层的分布主要受岩溶古地貌、风化壳层位及沉积相控制。

    The distribution of Caledonian residuum reservoirs in the south of Ordos Basin is mainly controlled by karst palaeogeomorphology, strata of residuum and sedimentary facies.

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  • 区域内水源丰富,有古洋水库、东溪水库、天然温泉和玉塔矿泉水,可提供充足的工业和生活用水。

    The water source is abundant, Guyang reservoir, Dongxi Reservoir, natural hotspring, and Yuta mineral water are able to supply enough industrial and living water.

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  • 尝试恢复东菲律宾海新型深水水成富铁锰结壳典型样品生长过程中所记录的古海洋环境。

    We attempt to recover the paleoenvironments recorded in the accretion of a typical new-type hydrogenetic ferromanganese crust from the deep water areas of the East Philippine Sea.

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  • 加里东期在东秦岭—大别造山带南侧江汉平原地区存在一个继承性古隆起,前人所称的“鄂中古陆”是其具体的表现。

    There is a inherited paleouplift in the Jianghan Plain area of the southern margin of East Qinling and Dabie Orogenic Belt during Caledonian period.

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  • 东濮凹陷在古近纪为断陷盆地,新近纪为坳陷沉积。

    Dong-pu Sag is a fault basin in palaeogene, with overlying depressed-type sediments in Neogene.

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  • 区内下古生界烃源岩经历了两次成油过程,第一次发生在加里东运动前的盆地沉降阶段,第二次发生在加里东运动后晚古生代陆表海沉积阶段。

    The first was in the basin subsidence stage that was prior to the Caledonian movement. The second took place in the marginal sea deposition stage after the Caledonian movement.

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  • 在此基础上探讨了东秦岭古生代古地理变迁过程。

    On this basis the paleogeographical changing process during the Paleozoic in the eastern Qinling is discussed.

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  • 下古生界在加里东运动暴露期间,黔中隆起及周缘盖层化学损失量巨大。

    The loss amount of caprocks was huge because of the exposure and chemical erosion during the Caledonian tectonic movements around the upheaval in the middle of Yunnan province.

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  • 东昆仑造山带基底主要形成于古元古代晚期。

    The basement of EKOB formed in late Paleo-Proterozoic.

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  • 东昆仑造山带基底主要形成于古元古代晚期。

    The basement of EKOB formed in late Paleo-Proterozoic.

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