寒武系 — 奥陶系源岩含油气系统是塔北地区最重要的一类已知含油气系统.
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The Tahe reservoir Ordovician carbonate rock belongs to the type reservoir that this is special.
塔河油田奥陶系碳酸盐岩属于该特殊类型油藏.
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明确了研究区奥陶系储层为超低基质孔的致密碳酸盐岩,岩溶作用为本区储层发育的主控因素.
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NOTES ON THE GENUS REEDOCALYMENE KOBAYASHI, 1951 ( TRILOBITA, ORDOVICIAN )
论奥陶纪三叶虫属ReedocalymeneKobayashi, 1951 ( 英文 )
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塔河油田奥陶系碳酸盐岩地层的主要储集空间为溶蚀缝、洞.
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寒武系和奥陶系是四川盆地乐山 — 龙女寺古隆起区的重要勘探目的层系.
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The main water source is fracture-karst water in Middle Ordovician carbonate rocks.
主要的供水水源为中奥陶统碳酸盐类岩石中的裂隙 - 喀斯特水.
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华南扬子区不同地点奥陶纪的岩相 、 生物相变化显著.
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There is abundant karst fissure water in the limestone and dolomite of Cambrian and Ordovician.
寒武系、奥陶系地层主要为灰岩和白云岩,其间赋存有较丰富的岩溶裂隙水.
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A rift trough along Mianxian-Lueyang ophiolitic melange belt was formed from Ordovician to Silurian.
奥陶纪—志留纪大致沿勉略构造带形成南秦岭裂陷槽.
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The Cambrian-Ordovician strata in Luxi Block are very continuous and well exposed.
鲁西地块的寒武 - 奥陶纪地层出露连续,露头较好.
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Among the multi-oil-generating beds, the Cambrian and Ordovician is the best one.
特别是在盆地内发现的多套生油层系中, 寒武──奥陶系为最佳.
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The Lower Ordovician in Tazhong area is dominated by marine carbonate.
塔里木盆地塔中地区下奥陶统主要为一套海相碳酸盐岩.
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Study of the Fluctuation of Sea Level During Ordovician Period in Tarim Basin
Hypermecaspis(三叶虫)的蜕壳塔里木盆地奥陶纪海平面变化
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Development Pattern and Distribution Rule of Source Rock of Cambrian-Ordovician in Tarim Basin
塔里木盆地寒武系&奥陶系烃源岩发育模式及分布规律
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伸展断裂系统发育于寒武纪、奥陶纪、早志留世、中-晚侏罗世和古近纪。
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Study on Eustatic Sea-Level Change Rule in Cambrian-Ordovician in Tarim Basin
塔里木盆地寒武&奥陶纪海平面升降变化规律研究
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