1.
CORRESPONDING CHRONOGENESIS BETWEEN THE MESOZOIC METALLOGENY AND MAGMATIC ACTIVITY IN NORTHEAST CHINA
东北地区中生代区域成矿与岩浆活动时序特征
2.
From Archeozoic to Cenozoic, there were magmatic actions in occurrence during every period.
从太古代到新生代,几乎各个时期都有岩浆活动。
3.
The Influence of Magmatic Activity on the Alteration of the Sandstone in the Petroleum-bearing Basin;
含油气盆地中岩浆活动对砂岩的改造
4.
Magmatism of the Western Chinese Altai Orogen: Geochronology, Petrogenesis and Tectonic Implications;
阿尔泰造山带西段岩浆活动的时代、成因机制及其构造意义
5.
Mesozoic Structural-Magmatic Activites and Mineralization in Beishan Region
北山地区中生代构造-岩浆活动与成矿
6.
ON THE TECTONIC ENVIRONMENT OF MAGMATISM IN YULONG PORPHYRY COPPER BELT, EASTERN TIBET
论藏东玉龙斑岩铜矿带岩浆活动的构造环境
7.
2. Andes magmatism and its tectonic setting; 3. Granites and geodynamics processes;
2.安第斯山岩浆活动及大地构造环境:3.花岗岩及地球动力学过程;
8.
Igneous activity had ceased by the beginning of the Tertiary period, 60million years ago.
6000万年前的第三纪初期，岩浆活动已经停止。
9.
Mesozoic Magmatic Activity and Middle-Cenozoic Basins of the Lower Reaches of Yangtze River
长江下游中生代岩浆活动与中新生代盆地
10.
Post-collisional Magmatism in Sawu'er Region, West Junggar, Xinjiang, China;
新疆西准噶尔萨吾尔地区后碰撞岩浆活动研究
11.
Alkali-rich Magmatism and Au-polymetal Metallogenic System in Northwestern Yunnan;
滇西北富碱岩浆活动与金多金属成矿系统
12.
The Research on the Tibetan Plateau s Cenozoic Magmatism Based on GIS;
基于GIS的青藏高原新生代岩浆活动的研究
13.
Structural Features and Magmation & Hydrothermalism in Chuxiong Basin;
楚雄盆地构造特征与岩浆活动及热液作用
14.
Magmatic Activity and Metallogeny of Dong Ujimqin Banner, Inner Mongolia;
内蒙古东乌珠穆沁旗岩浆活动与金属成矿作用
15.
The Late Mesozoic Magmatism Along the South Segment of the Tan-Lu Fault Zone and Its Implication for Lithospheric Thinning;
郯庐断裂带南段晚中生代岩浆活动及其对岩石圈减薄的指示
16.
Research on early cretaceous magmatic activity in the middle-southern segment of the Tan-Lu fault zone and its evolution
郯庐断裂带早白垩世岩浆活动与断裂带的活动关系
17.
general loader activity time limit
通用装入程序活动时限
18.
Similarly, high heat flows are to be expected among the active or not-too-long extinct magmatic belts of plate approximation zones.
同样，在板块相互靠近的地带的活动岩浆带或熄灭不久的岩浆带中也可以出现高热流。