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碳酸盐岩

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According to the lithologic and electric response character, the carbonate reservoir in this area can be classified into four types: vuggy reservoir, fractured reservoir, fractured and vuggy reservoir and cavernous reservoir.

根据储层岩电特征的差异,将轮古西地区碳酸盐岩储层划分为孔洞型、裂缝型、裂缝—孔洞型及洞穴型四种类型。

Richment organic material in the MT carbonates, and that may be a good potential petroleum resources.

MT碳酸盐岩中含有丰富的有机质,可能是好的潜在油气源岩。

There are two kinds of hydrocarbon regeneration: one is tectonic movement hydrocarbon regeneration and the other is deep-buried hydrocarbon regeneration.

塔中地区下古生界碳酸盐岩烃源岩中的干酪根、吸附有机质、包裹体有机质和晶包有机质,可以成为二次生烃的物质来源。

Hydrocarbon source rocks are distributed in craton basins and in-tracratonic rift basins.

碳酸盐岩是主要的储集层,泥质岩是主要的区域和局部盖层。

Aimed at the exploration of the lithostratigraphic reservoirs in four types of prototype basins(onshore terrestrial rifts,depressions,forelands and marine kratons)and in glutenites,volcanics and fracture-vug carbonate rocks,significant results are achieved on geological theory,technological innovation and production efficiency through fi...

针对中国陆上陆相断陷、坳陷、前陆和海相克拉通等4类原型盆地和砂砾岩、火山岩、缝洞型碳酸盐岩储集体中岩性地层油气藏的勘探,通过5年系统研究,在地质理论、技术创新与生产实效等方面取得重大成果:①系统建立了4类盆地岩性地层油气藏地质理论;②创建了中低丰度岩性地层油气藏大面积成藏理论;③创新了系统的岩性地层油气藏勘探程序与技术系列,自主创新21项核心专利;④推动了中国陆上由勘探构造油气藏向勘探岩性地层油气藏的重大转变,使中国石油天然气股份有限公司大规模岩性地层油气藏勘探取得显著成效。

The compaction released water karsts are formed under the middle-deep buried surroundings are a process of the dissolution role between compaction released water contained organic acid and carbonate rock, are final production of karstification roles.

鄂尔多斯盆地的压释水岩溶是在中深埋藏条件下,富含有机酸的压释水渗入碳酸盐岩含水层所产生的溶蚀作用过程及岩溶化结果。

The core issue is how to construct a reasonable physical, chemical and microbial condition for early rapid precipitation and filling of molar tooth cracks in the subtidal shallow marine.

在综述臼齿碳酸盐岩成因研究历程和国内外最新研究成果的基础上,总结评述了6种主要的臼齿构造成因模式,其核心问题是在元古代正常潮下浅海环境中构建成岩作用早期臼齿构造裂缝形成及等粒微亮晶方解石快速沉淀充填的物理、化学及微生物条件。

The Ordos Basin is a large-scale sedimentary basin in Northwest China. From bottom up, the hydrostratigraphic units in the basin are pre-Cambrian metamorphic rocks, lower-Paleozoic carbonate rocks, upper-Paleozoic to Mesozoic clastic rocks and Cenozoic deposits.

鄂尔多斯盆地是我国西北地区的大型构造沉积盆地,以前寒武系变质岩为基底,依次沉积了下古生界碳酸盐岩、上古生界一中生界碎屑岩和各种成因的新生界,总厚度达6000m。

The selenium contents in soils from Paleozoic Basalt and Red Earth Area of Carbonzte have the highest value. The selenium contents in soils from multi-Yellow-Red Earth, Purple Earth Clastic Yellow-Red earth and metamorphite red soil are lower than average value in China.

在各土壤类别中,玄武岩红壤和碳酸盐岩红壤,硒平均含量最高,而多源黄红壤、紫色土、碎屑岩黄红壤和变质岩赤红壤硒的平均含量均低于全国硒的背景值。

Carbonate rocks are susceptible to later recrystallization during deep burial, and can isotopically re-equilibrate with higher-temperature fluids depending upon the water/rock ratios and the isotopic composition of the fluids.

碳酸盐岩在深埋过程中很容易被后期的重结晶作用影响,并且在高温流体的加入时发生同位素的分馏,这种分馏与水/岩比率以及流体同位素的组成相关。

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