The Shengliqiao pluton in the western Kunlun Mountains is a composite batholith.
论证了西昆仑地区的胜利桥岩体是一个复式岩基。
The Fangshan granodiorite pluton of Lower Cretaceous occupies the middle of core.
核部有强力侵位的早白垩世的房山花岗闪长岩株。
The Shuanghe pluton is S-type granite and formed in the zone of the intercontinental collision.
双合岩体形成于板块碰撞同期，属S型花岗岩；
Yongtai stratigraphic sequence is a complex pluton, which is composed of 4 plutonic masses and 48 intrusives.
永泰序列系复式深成岩体，由4个深成岩体、48个侵入体组成。
Being an important pluton in the western part of Altay orogen, Tielieke pluton shows arc granitoid characteristics.
铁列克岩体是阿尔泰造山带西段的一个重要的岩体，显示弧花岗岩特征，其侵位时代一直没有解决。
The contact deformation shows that the Fenghuangshan pluton was controlled by a regional sinistral shear stress field.
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 Weipu granitic pluton and the Changpu migmatite are developed in the southern part of the Wuyi tectonic belt, South China.
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 Fenghuangshan pluton, which consists of granodiorite and quartz monzodiorite, is the main part of the Fenghuangshan ore field.
凤凰山岩体为凤凰山矿田的主要组成部分，主要岩石类型为花岗闪长岩、石英二长闪长岩。
Therefore, fluids that are brought by the Xiangshan pluton from the mantle source region are rich in H2O and reductive volatiles CH4 etc.
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。
The Hueichizi granitic pluton consists mainly of granitoid rocks. which have in common deformation fabric and complicated deformation processes.
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 Penshan granitic body is a calc-alkaline pluton composed of Muscovite alkali granite, two-mica alkali feldspar granite and biotite adamellite.
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 geological characteristics, petrology, mineralogy and geochemistry of Ningshan granitic pluton groups in the south of east Qinling Orogen are dealt with in this paper.
本文详细研究了东秦岭造山带南部宁陕花岗岩体群的地质特征、岩石学、矿物学和地球化学特征。
The stitching pluton, intruded into main fault plane of collision zone, could be formed in syntectonic period and also in the period of subsequent collision, i. e. post collision.
沿碰撞带主断层面贯入的“钉合岩体”可以是同构造期形成的，也可能是继续碰撞作用的产物。
The deformations of the pluton indicate the characteristics and strength of the regional deformations during the Jinning period, and constrain the period of its strongest deformation.
该岩体的变形揭示了该区晋宁期区域变形的特点和强度，并限定了其峰期变形时间。
The deformations of the pluton indicate the characteristics and strength of the regional deformations during the Jinning period, and constrain the period of its strongest deformation.
该岩体的变形揭示了该区晋宁期区域变形的特点和强度，并限定了其峰期变形时间。
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