花岗斑岩

通过矿区的岩石样品分析，确定含矿热液是来自于燕山期中侏罗世花岗斑岩。

The ore-bearing hydrothermal fluid produced from the Yanshan granite porphyry Jurassic period is determined through the analysis of rock samples in the mining .

铅锌矿石既与火山喷流沉积作用有关，又与花岗斑岩侵入作用有关，显示混合成因。

Lead-zinc ore related to volcanic effusion deposition and granite porphyry intrusive , display mixing origin .

花岗斑岩类岩石中Au、Pd溶解性状的实验研究

Experimental research on dissolution properties of Au and Pd contained in granite-porphyry

研究花岗斑岩类岩石中Au、Pd的溶解性状，对于研究其溶解、迁移、沉淀条件有着重要的理论价值。

The research on dissolution properties of Au and Pd contained in granite-porphyry is of great significance for the study of conditions under which Au and Pd dissolve , migrate and deposit .

内蒙古白音宝力道花岗斑岩锆石U-Pb定年&白音宝力道金矿成矿主岩的形成时代

Zircon U-Pb dating of the Bayan Bold granite-porphyry in Inner Mongolia : The age of the host rock of the Bayan Bold gold deposit

花岗斑岩和火山岩的KAr同位素为83～138Ma。

K / Ar isotope age from granite-porphyry and volcanic roks are 83 ~ 138 Ma .

主要含矿角砾岩的RbSr同位素等时线年龄为191Ma，两期隐爆角砾岩之间侵入的二长花岗斑岩脉的等时线年龄为177Ma。

The Rb-Sr isochron age of early ore-bearing breccia is 191 Ma , and the age of monzonitic granite porphyry emplaced after the early breccia pipe is 177 Ma .

斜长花岗斑岩为地壳重熔型花岗岩，具多期次性；

Plagiogranite porphyry is crustal anatectic granite formed by multiple intrusions .

斑岩型金矿床，矿体赋存于花岗斑岩和花岗质侵入岩中；

Porphyry gold deposits , ore-bodies are hosted in granite-porphyry and granite-plutons ;

苏州印支期花岗斑岩的地球化学特征及其成因探讨

Geological character and genesis of Indian granite porphyry in Suzhou

热储由中生代燕山期花岗斑岩、凝灰岩组成。

Its heat reservoir is composed of Yanshanian granite-porphyry and tuff of Mesozoic .

浙江桐庐自碎二长花岗斑岩的特征和成因

The characteristics and the origin of the autoclastic monzonitic granite-porphyry , Tonglu , Zhejiang

试论凝灰熔岩碎斑熔岩花岗斑岩的成因联系

The relationship of tufflava-porphyroclastic lava - granitic porphyry

我国花岗斑岩中的铅猛钛铁矿

Senaite present in granite porphyry of China

喜山早期黑云母花岗斑岩、强硅化花岗斑岩是区内斑岩型铜、钼矿床的成矿母岩。

The metallogenic rock are biotite and intense-silicified granite-porphyry of the early stage of Xishan .

浅部石英斑岩为含矿岩体，深部花岗斑岩为矿源岩体。

The shallow quartz porphyry is ore-bearing massif and the deep granite porphyry is ore-origimating one .

辉绿岩、煌斑岩、花岗斑岩及石英脉形成于华力西期以后。

The diabase , lamprophyre , granite porphyry and quartz veins are formed after Variscan period .

巴泉铀矿床花岗斑岩中的交代钠长岩及其演化特征

The character of metasomatic albite and its evolution in granite - porphyry in Ba Quan uranium deposit

第一阶段有花岗斑岩、石英斑岩两次侵入；

In the first stage , there are two times of intrusions , granite-porphyry and quartz-porphyry intrusions .

矿床赋存于中生代早白垩世火山岩、次火山岩内，矿体产于北东向花岗斑岩脉中，且严格受火山构造控制。

All ore veins are confined in the granitic porphyritic dikes and strictly controlled by volcanic structures .

吉林正岔铅锌矿床是与燕山期花岗斑岩有关的夕卡岩铅锌矿床。

The Zhengcha lead-zinc deposit , Jilin , is a skarn-type lead-zinc deposit associated with Yan-shanian granite-porphyry .

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 .

花岗斑岩是钼矿床的矿质的主要来源，钾长石是主要的载体矿物。

Porphyry granite is the main mineral sources of molybdenum deposit , potassium feldspar is the main carrier mineral .

其成矿物质主要来源于花岗斑岩，该矿床是与陆壳重熔型花岗岩类斑岩体有成因联系的斑岩型锡矿床。

It is suggested that this porphyry tin deposit is genetically related to continental crust remelted granite - porphyry .

华北地台南缘燕山期花岗斑岩类小岩体形成于大陆板内环境，它具有类似岛弧&活动大陆边缘钙碱系列岩石地球化学特征，其成分在空间上呈现极性特征。

The Yanshanian granite - porphyries along the southern margin of North China Craton were developed in an intraplate environment .

两矿床的矿体主要赋存在花岗斑岩及其与围岩的接触带中。

The mineral-bodies of the two mineral deposits are mainly existed in the contacting zone of granite-porphyry and adjoining rock .

岩体的岩石地球化学研究并与金堆城钾长花岗斑岩比较，二者同是燕山期岩浆活动的产物；

Study on the lithogeochemistry and its correlation to Jinduicheng granite indicate that they are all products of Yanshanian magmatism .

小康锰银多金属矿受下三叠系溪口组地层、断裂构造破碎带和花岗斑岩接触带控制，主要围岩蚀变有矽卡岩化、角岩化。

Xiaokang Mn-Ag multi-metal mine is controlled by structural broken belt and granite-porphyry contact zone of xikou formation of lower-T system .

福州屏山苔泉的成因及其对花岗斑岩残积土岩土力学性质的影响

Fuzhou Pingshan " liver moss spring " origin and its to granite - porphyry remnant fill crag soil mechanics nature influence

新宁&灰汤断裂带花岗斑岩与煌斑岩脉的分布特征及其找矿意义

The distribution feature of granitic porphyry dyke and lamprophyric dyke along xinning & huitang fracture zone and its significance for prospecting