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产出于岩石圈伸展拉张环境。It is suggested that the pluton formed in lithosphere extension environment.
岛弧深成岩成分变化较大,由闪长岩变化到花岗岩,成岩时代为奥陶纪。Island-arc pluton consists of diorite to granite, which formed in Ordovician.
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论证了西昆仑地区的胜利桥岩体是一个复式岩基。The Shengliqiao pluton in the western Kunlun Mountains is a composite batholith.
核部有强力侵位的早白垩世的房山花岗闪长岩株。The Fangshan granodiorite pluton of Lower Cretaceous occupies the middle of core.
湘南骑田岭岩体主要由两阶段侵位所形成,早阶段侵位花岗岩组成骑田岭岩体的主体。Qitianling pluton was formed by two phases of emplacement, and is mainly composed of early stage granite.
湖南骑田岭岩体主要由两阶段侵位所形成,早阶段侵位花岗岩则组成骑田岭岩体的主体。The Qitianling pluton was formed by two phases of emplacement, and is mainly composed of early stage granite.
小白石头黑云母花岗岩位于中天山地块东部南缘。The Xiaobaishitou biotite-granite pluton is situated in the southeastern margin of the central Tian Shan block.
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接触带构造变形特征显示岩体侵位受控于区域左旋剪切应力场作用。The contact deformation shows that the Fenghuangshan pluton was controlled by a regional sinistral shear stress field.
西昆仑山阿卡孜岩体是该区已知的最古老侵入体。Akazi pluton, which occurs in Western Kunlun in north of Qinghai-Tibet plateau, is the known oldest pluton in this area.
乳山金矿床位于牟平-乳山金矿带中部的昆嵛山花岗岩体内,是胶东近年来探明的一个重要石英脉型金矿床。The Rushan gold deposit, one of the important quartz-vein type gold deposits, is located in the Kunyushan granitic pluton.
闽西玮埔岩体和赣南菖蒲混合岩位于武夷山构造带南部地区。The Weipu granitic pluton and the Changpu migmatite are developed in the southern part of the Wuyi tectonic belt, South China.
该岩体主要由细粒纯橄榄岩、中粗粒纯橄榄岩和斜辉橄榄岩组成。The pluton is composed mainly of fine grained as well as medium-and coarse-grained dunite and plagioclase-pyroxene peridotite.
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在对陕西宝鸡一带进行地质大调查时,发现北秦岭造山带西段的唐藏石英闪长岩体具有埃达克岩的特征。The Tangzang quartz-diorite pluton which has the characteristics of Adakite was founded in a geological survey in Baoji, Shaanxi.
骑田岭花岗岩是燕山早期深源浅成的高钾钙碱性复式花岗岩岩体。Qitianling granite is a post- collisional , deep-sourced and hypabyssal, early Yanshanian high-K calc-alkaline granite complex pluton.
因而,香山岩体所携带的流体是一种富CH4等还原性挥发份和富H2O的流体。Therefore, fluids that are brought by the Xiangshan pluton from the mantle source region are rich in H2O and reductive volatiles CH4 etc.
灰池子复式岩体是北秦岭加里东造山带规模最大的花岗岩体,其成因争论较大。Huichizi complex pluton is the largest scale granitoid pluton of the north Qiniing Caledonian orogenic zone, and its genisis is a controversy.
骑田岭岩体是南岭地区燕山早期具幔源组分贡献的花岗岩典型代表。The Qitianling pluton is one of the typical granites with the contribution of mantle-derived components in the Nanling region, southern China.
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打鼓寨岩体及近外围特别是其东北部是进一步开展铀矿勘查工作的方向。The authors consider Daguzhai pluton and the near periphery, especially its northeast part, as the prospecting target for further exploration.
灰池子岩体主要由花岗岩类岩石组成,该岩体岩石普遍具变形结构,变形过程较复杂。The Hueichizi granitic pluton consists mainly of granitoid rocks. which have in common deformation fabric and complicated deformation processes.
彭山岩体是由白云母碱长花岗岩、云母碱长花岗岩和黑云母二长花岗岩组成的钙碱性花岗复式岩体。The Penshan granitic body is a calc-alkaline pluton composed of muscovite alkali granite, two-mica alkali feldspar granite and biotite adamellite.