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On the basis of the study on the lithology, rock, analyzed the affecting factorof the causes of volcanic reservoir.

在岩性、岩相研究的基础上,分析了火山岩储层成因的影响因素。

Analysis of their morphologies and features leads to the conclusi on that these structures might have been in connection with metazoan activity, bu t the possibility of their abiotic origin can not be ruled out.

通过对上述构造形态和特征分析,这些构造可能与后生动物的活动有关,但也不排除它们是非生物成因的可能。

The monazite samples of various genetic types are taken fro m different localities in China and have been analysed by EPMA.

采用电子探针分析研究了花岗岩、伟晶岩和热液交代等三种不同成因的独居石微粒微区成分分布的特征。

Study on the lithology and petrology (fine-grained cold-quenching ring of the enclaves, the reverse vein, the complex enclaves, the plagioclase phenocryst from both host rock and enclaves that is consist on the crystal form, composition and light, et al.), petrogeochemistry (Y/Nb=2.77~6.82, La/Nb=0.91~4.33, Ba/Nb=0.13~37.86, et al.), Sr and Nd isotope most ISr between 0.7031~0.7041,εNd(t=5.2~7.1 and LA-ICP-MS zircon U-Pb dating (the host rock age is 311±12Ma, and enclaves is 306±7Ma), believe the Huangyangshan pluton is crust-mantle hybrid genesis.

通过岩石学和岩相学(包体细粒淬冷边,反向脉,复合包体以及寄主岩石和包体中斜长石斑晶在形态、成分、光性上的一致性等),岩石地球化学(Y/Nb=2.77~6.82,La/Nb=0.91~4.33,Ba/Nb=0.13~37.86等),Sr和Nd同位素(ISr多数在0.7031~0.7041,εNd在5.2~7.1之间)以及LA-ICP-MS锆石U-Pb测年(寄主岩石为311±12Ma,包体为306±7Ma)综合研究认为黄羊山花岗岩是壳-幔源岩浆混合成因的

The objection to the placer origin have centred around the softness of uranium compounds.

反对砂矿成因的论据主要是:铀的化合物不耐磨蚀。

The trap contains sand lentoid traps formed by sand bar and sand updipwedge-out traps.

发育的地层—岩性圈闭类型主要为砂质滩坝成因的砂岩透镜体岩性圈闭和砂岩上倾尖灭地层圈闭。

The trap contains sand lentoid traps formed by sand bar and sand updip wedge-out traps.

发育的地层—岩性圈闭类型主要为砂质滩坝成因的砂岩透镜体岩性圈闭和砂岩上倾尖灭地层圈闭。

In addition to Fe+(54Fe+, 56Fe+, 57Fe+), other fragment ions were detected in bacteriogenic pyrites, such as 27 Al+, Si+(28Si+, 29Si+, 30Si+), 40Ca+, Cu+(63Cu+, 65Cu+), Zn+(64Zn+, 66Zn+, 67Zn+, 68Zn+), Ni+(58Ni+, 60Ni+, 62Ni+), and C3H7+.

在杆状菌落成因的黄铁矿中,检测到的组成有 Fe+(54 Fe+、56 Fe+、57 Fe+)、 27 Al+、 Si+(28 Si+、29 Si+、30 Si+)、40 Ca+、 Cu+(63 Cu+、65 Cu+)、 Zn+(64 Zn+、66 Zn+、67 Zn+、68 Zn+)、 Ni+(58 Ni+、60 Ni+、62 Ni+)、 C3H7+。

The authors try to use conceptual model,mathematical model and computer model to reconstruct the formation and evolution of dynamic geomorphic features of tectonic gulches.

尝试从概念模型、数学模型、计算机模型等多个层次构建构造成因的沟谷形成、演变的动态地貌模型。

The minerals of microbial genesis are generally characterized by small grain size and/or unique isotopic features.

微生物成因的矿物总体来说颗粒都很小和/或有着独特的同位素特征。

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