矿石铅同位素模式年龄和石英斑岩体侵入年龄的一致性反映燕山期构造、岩浆和成矿作用的密切关系。
Consistence between isotopic model age of lead ore and intrusion age of quartz porphyry shows close relations among structure movements, magmatism and mineralization in Stage of Yenshan.
明确提出了侵入接触带构造控矿的观点，从而为进一步研究其成矿及控矿作用提供必要的理论依据。
The idea that the intrusive contact structure controls the-body will provide theoretical evidence for the further research of mineralization and ore control.
地层、侵入岩、断裂构造是工作区内钨矿的三个基本的成矿地质条件。
The stratum, intrusive rock, and faulted structure are three basic ore-forming geology factors of tungsten ore in the work area.
岩浆岩的侵入明显受断裂构造控制。
Magmatic intrusion obviously is controlled by faulted structure.
富硅灰岩-三叠世侵入岩-构造裂隙系统是主要控矿因素。
The main ore controlling factors are wollastonite rich rocks, Tertiary intrusive rocks and structural fissures system .
北秦岭侵入岩带与同时代的蛇绿岩带有力地证明，北秦岭晋宁运动的构造体制是板块体制。
The intrusive rock belt and the ophiolite belt of the same time together demonstrate that the tectonic system of the North Qinling during the Jinning movement is plate tectonic system.
寒山大型金矿是近年来在北祁连山西段发现的与侵入岩有关的构造蚀变岩型金矿。
The Hanshan gold deposit is a tectonic altered rock type deposit discovered recently in North Qilian Mountains.
同时，侵入岩浆的强烈活动也是本区构造环境由挤压向伸展转换的标志。
The intrusive magmatic activities were indicators of the tectonic setting which changed from compression to extension.
结合台马碎斑熔岩与周边火山岩、侵入岩、地层的关系，认为它是早—中三叠世中心裂隙式火山构造中央部位侵出的穹状岩脊。
Combined with the surrounding volcanic rocks, intrusive rocks and strata, the Taima rock body is considered as a dome of the central part of the central fissure type volcanic structure.
影响储集空间发育的因素主要包括构造运动、断裂、岩性、火成岩侵入体以及剥蚀程度等方面。
Influence factors of reservoir Spaces are summarized, including tectonic movement, fault, lithology, volcanic intrusions and denudation degree, etc.
矿区内闪长岩近东西向侵入上石炭统奇尔古斯套组上部，构造破碎作用严重。
In mining area, nearly east-westward Diorites body invaded to upper rocks of Qiergustao formation, and was fragmentated serious.
侵入岩带和每个侵入岩体的产状都大致与西北向的周围构造协调。
The zone of the intrusions as well as the attitude of the individual bodies harmonizes broadly with the steep northwesterly structure of the surroundings.
形成这样的地质环境条件主要是岩浆侵入作用导致上覆火山岩的褶皱构造、侵入体的岩穹构造及接触破碎带构造等。
The geologic environment was mostly resulted from the intrusion of magma which led to folding of the overlying volcanic series, the formation of the intrusive dome and the contact broken zone.
由于燕山晚期岩浆岩的侵入及锡矿山背斜的形成，在背斜两翼产生重力滑动构造。
Thrust and gravity gliding structures are both developed in the west of Lianyuan depression.
岩墙群的构造形态和流动构造表明鲁西基性岩墙群是基性岩浆侵位到先存的张性破裂中的产物，岩墙自北部向南部侵入。
The flow structures and geometry evidences of the dykes indicate that the magma source of these dykes intruded the pre-existing tensional rupture.
由于燕山晚期岩浆岩的侵入及锡矿山背斜的形成，在背斜两翼产生重力滑动构造。
Because of the magmatite intrusion in Late Yanshan period and the formation of Xikuangshan anticline, gravitation gliding structures are developed at the both wings of the anticline.
依据不同构造岩浆区单元，江西中南部中新元古代-晚三叠世的侵入岩可划分为武夷山构造岩浆区、赣西南构造岩浆区。
The intrusive rocks from middle-late proterozoic to late triassic in middle-south Jiangxi province can be divided into two tectonic-magma areas of Wuyishan and south-west Jiangxi.
以北山东段岩性构造填图酸性侵入岩分类为例，介绍航空物探岩性分类的技术方法及工作要点。
The results obtained can also provide new information for geological exploration. This paper describes briefly the mapping of acid intrusive rocks in eastern Beishan area.
研究区内西南部区域高异常在剖面图上其走向与逆冲推覆构造走向基本一致，推测异常是由逆冲构造引起，也可能是盖层中侵入岩引起。
The trend of the high anomaly in south west area of the study region is basically same with the thrust fault, so we infer that the anomaly is caused by it.
依据不同构造岩浆区单元 ，江西中南部中新元古代 -晚三叠世的侵入岩可划分为武夷山构造岩浆区、赣西南构造岩浆区。
The intrusive rocks from middle-late proterozoic to late triassic in middle-south Jiangxi privince can be divided into two tectonic-magma areas of Wuyishan and south-west Jiangxi.
依据不同构造岩浆区单元 ，江西中南部中新元古代 -晚三叠世的侵入岩可划分为武夷山构造岩浆区、赣西南构造岩浆区。
The intrusive rocks from middle-late proterozoic to late triassic in middle-south Jiangxi privince can be divided into two tectonic-magma areas of Wuyishan and south-west Jiangxi.
应用推荐