• Study has shown that the primary rocks of metamorphic supercrustal rocks are mainly calc-alkaline volcanic rocks.

    研究表明变质上壳岩原岩主要以钙碱性火山(熔)为主。

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  • The primary rocks are a series of intermediate-acid volcanics and carbonate formed in environment of rift valley.

    裂谷环境下形成酸性火山岩碳酸盐岩。矿体的容矿岩石是镁质大理岩。

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  • The primary rocks include the various sodium-rich volcanic rocks and the sedimentary rocks with sodium-rich volcanic materials which are well developed in the North Qilian eugeosyncline area.

    区内含蓝闪石岩包括优地槽内发育各类火山岩、含富钠火山质的沉积岩

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  • Using some samples' kinetics parameter to the Permian source rocks of northeast of Sichuan Basin, simulates the primary hydrocarbon generation history and calculates hydrocarbon generating quantity.

    一些样品动力学参数运用于东北地区叠系模拟初次生过程,进行初次生烃量计算。

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  • The compactionand secondary enlargement of quartz lead to the great decrease of primary porosity of clastic rocks, and dissolution is contributed to the formation of secondary pore space.

    压实作用和石英次生加大使碎屑原生孔隙极大降低溶解作用次生孔隙形成的主要因素。

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  • In the southern North China, the lower Paleozoic source rocks reached primary maturation at late Triassic and the secondary hydrocarbon generation did not occur at the Cenozoic.

    华北地区古生界烃三叠世达到早成熟阶段,新生代基本发生二次生作用。

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  • The result of the primary migration simulation suggests that there are different carbon isotopic fractionation effects in the primary migration of different source rocks.

    通过初次运移模拟实验证明了烃类不同类型烃源岩发生初次运移能够产生不同程度物理同位素分馏效应;

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  • This is attributable to the preservation of a part of the primary porosity in the rocks due to the formation of high porosity pressure.

    这种现象产生原因保持一部分原有孔隙度,而保持孔隙度控制因素是形成孔隙压力。

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  • The extent of ree enrichment and differentiation is affected by ree concentrations and distributions in the primary granitoid rocks, weathering degree, etc.

    REE风化壳中富集分异风化壳发育程度、花岗岩ree含量及其分布分配的影响。

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  • There are primary stylolite and secondary stylolite in sedimentary rocks.

    沉积岩中的缝合线构造原生次生两种成因。

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  • The studied results show that different secondary changes occurred in fluid inclusions of various rocks and no primary inclusion has been found.

    研究结果表明各类相岩石的流体包裹体均程度不同发生了次生变化发现原生包裹体。

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  • The heterogeneity and micro-fissures in source rocks are unfavorable to primary migration of oil and gas, which retained some oil gas within the source rocks forever as micro-reservoirs.

    岩层的均质性裂缝初次运移十分不利它们油气滞留在源岩层使其成为微油藏

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  • In the research area, the primary surface formation are the Archeozoic - Proterozoic Jiaonan group there are kinds of Clastic rocks and Volcanic rocks in the metamorphite and Mesozoic Cretaceous.

    研究区内出露地层太古界——元古界胶南各类变质中生界白垩系各类碎屑岩和火山岩为主。

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  • The primary and secondary pores of volcanic rocks provided reservoir space there. Volcanic rock may become cap rock under certain conditions.

    火山岩原生次生孔隙使成为储集层,在一定条件下可成为层。

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  • Volcanics mainly growth gas pocket, primary rift and secondary rift, The secondary porosity of clastic rocks is much more developed.

    火山岩储层主要发育气孔、原生裂缝次生裂缝;碎屑岩则以次生孔隙为主

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  • The results show that the siliceous rocks intercalated with the coal seams were deposited from a hydrothermal medium through which germanium was enriched in the coal beds. The primary source...

    研究结果表明矿化煤层互层热水沉积成因,矿化煤层中的主要来自形成硅质岩的热水溶液,这种热水溶液中的锗则主要由盆地基底的锗花岗岩所提供。

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  • Sedimentation controlled the textures of clastic rocks such as matrix, sorting and rounding, and further affected the texture of primary pores, which served as basement for later dissolution.

    沉积作用控制碎屑岩杂分选磨圆结构特征,进而控制了原生孔隙结构后期溶解作用形成奠定了基础

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  • Moreover, the microorganism which was brought by permeable surface water degraded the primary kerogen in sedimantary rocks and could produce reducing matters. The precipitation and th…

    同时地表下渗的大气降水携带了细菌类微生物原生有机质进行生物降解生成硫化氢类还原物质

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  • Moreover, the microorganism which was brought by permeable surface water degraded the primary kerogen in sedimantary rocks and could produce reducing matters. The precipitation and th…

    同时地表下渗的大气降水携带了细菌类微生物原生有机质进行生物降解生成硫化氢类还原物质

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