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The metamorphic grades of Minleh and Changma areas are prehnite-pumpellyite and prehnite-actinolite facies, respectively.

民乐与昌马地区变质火山,变质度分别葡萄石-绿纤石相葡萄石-阳起石相。

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The sediments are detrital and largely of greywacke facies.

屑质,大部分属于杂质砂相。

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Coal-bearing strata belong to Middle-Lower Jurassic Series Jiangcang Formation,coal-forming environment was Mesozoic faulted basin fluviolacustrine,bog facies.

含煤地层中下侏罗统江仓组,成煤环境属中生代断陷盆地内河湖、沼泽相积。

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Inland foraminifer fossils are considered as one of good indicators of marine facies.

内陆有孔虫化石群被一些学者视是海侵或残留海的指相化石。

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Shanxi Formation is a set of paralic continental deposit,of which,fluvial,swamp and lacustrine facies alternatively presented regularly.

山西组一套近海的陆相积,其中河流相、沼泽相及湖泊相有规律地交替出现。

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Golden minerals in Carlin-type gold ore are dominated by native gold and argentiferous native gold of Au-Ag series, havehigh fineness,and are mainly enriched insulfide facies.

卡林金矿的载金矿物主要黄铁矿粘土矿物,其次是毒砂石英。

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The sedimentary facies in Heshilafu is an alluvial fan - fan delta -lake systetn, and it can be further devided into several parfacies including microfacies.

什拉甫地区积相冲积扇──扇三角洲──湖泊积体系,进一步分几种亚相微相

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Dissolution is controlled by both sedimentation and tectonization, and the converted degree on reservoirs is closely related to sedimentary facies and the distance from unconformity interfaces.

溶解作用受构造作用的控制,其对储层的改造程度与积相带及距不整合面的距离密切相关。

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After rapid overall swelling , in the late stage occurred alluvial fan-braided river facies sedimentary cycles made of red polyterrigenous molasse deposit s with multi-source supplying.

晚期全区讯速台升,形成冲积扇~辫状河流相的磨拉石红色复陆屑积旋回及多物源供应格局。

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The former three stages reflect the major process of eclogite facies metamorphism and the latest stages the light overprinting of greenschist facies retrometamorphism at the shallow level of crust.

前三个阶段反映了榴辉相变质作用的主要过程。后一阶段,反映了榴辉在地壳浅部层次绿片相环境下遭受轻微的叠加改造。

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To date, komatiites with spinifex textures have not been found in the supracrustal rocks, but rock sequences similar to greenstones metamorphosed up to upper amphibolite facies are often observed.

在龙岗地块与北带之间的接触带上,发育了一条晚太古宙-古元古宙时期的线性活动带。

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Site soils in southern area of Jiangsu province belong to washland sediment or limnetic facies sediment.The components of sediment are very complex and process of sedimentation is in disorder.

苏南地区场地土主要漫滩相、湖沼相或冲湖相新近积软弱土,结构松散,积零乱,成分复杂,饱水可液化粉细砂层及粉土层较发育,在地震或动力荷载的作用下有可能发生软土震陷或砂土液化。

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Its original rock is sedimented in the environment of active epicontinent-seaboard with basic volcanism, and become khondalite series through the Archean regional high-amphibolite facies metamorphism.

形成于具有基性火山作用的活动大陆边缘滨海-浅海环境。经过太古宙的区域高角闪相变质作用,形成孔兹系。

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