1.
Tectonic Environments of Granitoids in the West Kunlun Orogenic Belt
西昆仑造山带花岗岩形成的构造环境
2.
A preliminary study of the relationship between granitoids and the growth of continental crust:a case study of the formation of key orogen granitoids in China
花岗岩类与大陆地壳生长初探——以中国典型造山带花岗岩类岩石的形成为例
3.
GRANITE CLASSIFICATION,FORMATION,EVOLUTION AND MINERALIZATION IN THE WUGONG SHAN METALLOGENIC BELT
武功山成矿带花岗岩的分类、形成、演化与成矿
4.
Metallogenic significance and geochemical characteristics of granite rock from Yangshan gold ore belt Wenxian in Gansu province
甘肃文县阳山金矿带花岗岩岩石地球化学特征及其成矿意义
5.
The temporal and spatial evolution of orogenic granitic belt shows certain kind of regularities: subduction type granites→collision type granites→extensional type granites.
造山带花岗岩的时空演变规律是：俯冲型→碰撞型→伸展型。
6.
Ore-bearing rock body is located at the top of" magma tree" within the belt of dimicaceous granite-granitic pegmatite.
含矿岩体位于“岩浆树”顶端-二云母花岗岩-花岗伟晶岩带。
7.
A Study on the Geochemistry of the Rocks and Minerals in the Granite Depression Zones in the Gejiu Tin-polymetallic Orefield;
个旧花岗岩凹陷带岩矿地球化学研究
8.
The Mesozoic and Cenozoic plutonic intrusive rocks are grouped into the Lhagoi Kangri and Gangdise granite zones.
将中新生代深成侵入岩划分为拉轨岗日花岗岩带和冈底斯花岗岩带两个岩浆带;
9.
GEOLOGICA FEATURES OF THE CALEDONIAN GRANITE ZONE IN THE WEST KUNLUN AREA
西昆仑加里东期花岗岩带的地质特征
10.
"Mantle signature" on the Indosinian granitoid belt in South Qinling,Central China
南秦岭印支期花岗岩带的“地幔印记”
11.
Research on the Metallogenia of the Granite Contach-depression Zones in GeJiu Tin-copper Polymetallic Deposit;
云南个旧花岗岩凹陷带锡铜多金属成矿学研究
12.
Elemental Geochemistry and Petrogenesis of A-type Granites in the Sulu Orogen
苏鲁造山带A型花岗岩的元素地球化学及其成因
13.
Gneiss is called bastard granite.
片麻岩叫作粗花岗岩。
14.
Granite comes in large masses.
花岗岩形成巨大的岩体。
15.
granit is S-type and its evolution sequence might begranomonzonite → muscovite-granite(outcrop) → feldspar-granit →muscovite-granite(core);
花岗岩演化顺序可能为二长花岗岩→露头白云母花岗岩→钾长花岗岩→白云母花岗岩芯。
16.
GEOLOGY AND GEOCHEMISTRY OF ARCHEAN GRANITE-GREENSTONE BELTS IN NORTHERN LIAONING PROVINCE AND SOUTHERN JILIN PROVINCE
辽北－吉南地区太古宙花岗岩－绿岩带地质地球化学
17.
The mineral-bodies of the two mineral deposits are mainly existed in the contacting zone of granite-porphyry and adjoining rock.
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。
18.
Unit two belongs to late Archaean middle-low grade metamorphic rocks with the characteristics of granite -greenstone belt.
组合(2)是具花岗—绿岩带特征的晚太古代中、低级变质岩系.