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哈图金矿局岩浆期后中温热液矿床。Ha-Tu Gold Deposit is a postmagmatic mesothermal deposit.

它属于中温岩浆热液型矿床。The deposit belongs to the mesothermal magmatic-hydrothermal type.

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北京土壤温度属温性土壤温度状况。The soil temperature regime in Beijing belongs to mesothermal category.

金矿为浅-中深成矿的中温热液矿床。The deposit is a mesothermal gold deposit mineralized in shallow middle depth.

地幔流体的碱交代作用形成大型—超大型中高温热液矿床。The alkali metasomatism of mantle fluids forms large scale mesothermal deposit.

该矿床属岩浆期后中一低温热液充填一交代石英脉型金矿床。The gold deposit is a postmagmatic mesothermal -epithermal quartz-vein type gold deposit.

八卦庙金矿床是分布于秦岭造山带中的一种中高温碳酸盐型热液金矿床。The Baguamiao gold deposit in a sort of mesothermal hypothermal carbonate type gold deposit.

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五圩矿田各多金属矿床均为中—低温热液充填型脉状矿床。The polymetallic deposits are mainly epithermal to mesothermal filling deposits in the Wuxu orefield.

桃园钼矿床属中温热液脉型矿床,围岩蚀变具线型对称特征。Taoyuan molybdenum ore belongs to mesothermal hydrothermal vein deposit. Alteration of country rock has linear feature.

矿床可能与隐伏的燕山期细粒花岗岩、花岗斑岩岩脉有成因关系,属与燕山期岩浆活动有关的中-高温热液矿床。It is a mesothermal to hyperthermal deposit related to the blinded Yanshanian fine-grained granite or granite-porphyry dykes.

金厂金矿床是我国西南最大的与超基性岩有生因关系的中低温热液石英脉型金矿床。Jinchang gold deposit is one of the largest mesothermal deposits closly related to the ultrabasic rocks in South-West of china.

该矿是发现最早的破碎带蚀变岩型金矿床,其成因属重熔岩浆中温热液型。The mine is the earliest discovered broken belt altered rock type gold deposit, it belongs to remelting magma mesothermal type.

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一种自控恒温保温杯,其由杯体以及带螺纹的盖子和中温相变物质组成。A vacuum cup of automatic control of thermostat comprises a body, a cover with screw threads and a mesothermal phase-change material.

锶氧和铝同位素证据表明,这些金矿是海西期形成的岩浆热液金矿床。Sr-, 0- and Pb isotopic data indicate that they are of the type of magmatic mesothermal gold ore deposit formed during the period of Hercynian movement.

壤塘金矿是近期探明的一条中温热液型金矿成矿带。经研究发现其成矿作用与脆韧性剪切、脆性剪切变形密切相关。Ramtang gold belt is an extraordinary mesothermal gold metallogenetic belt whose genesis is related to brittle-ductile shear zone and brittle shear zone.

河东金矿床矿体呈完整、连续的透镜体,具有典型的中温热液矿物组合和围岩蚀变分带特征。Hedong"s gold body is fully continuous lens , has the characteristics of typical mineral assemblages of mesothermal ore deposit a nd zoning of wall-rock alteration."

胶东地区存在两种不同地质特征的脉型金矿———中深成热液脉型金矿与浅成热液脉型金矿。There exist two kinds vein gold deposits in different geological characteristics in Jiaodong Area, namely mesothermal vein gold deposit and epithermal vein gold deposit.

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并在此基础上,对矿床的成因机制及其演化过程作了详细分析,确定该矿床为中高温变质热液蚀变岩型金矿床。On this basis, the genetic mechanism and evolution of the deposit are detailed analysed. It is defined that the deposit is a metamorphic hydrothermal mesothermal altered gold deposit.

老厂式铅锌矿是产于泥盆系和寒武系不整合界面之间的脉状中温热液铅锌矿床,受断裂构造控制。Lead and zinc deposit of laochang type is mesothermal deposit of vein type that occur in an unconformity interface between Devonian and Cambrian strata and controlled by fracture structure.