1.
classification of in-situ rock
原地岩石的鉴定分级
2.
Exploring the reasons for karst collapse of geological disasters in the Longyan basin
龙岩盆地岩溶塌陷地质灾害原因探讨
3.
The Feature of the Metamorphite and the Photolyte Analysis on the Fuping Group in the Baoding Area;
保定地区阜平群变质岩岩石特征及原岩分析
4.
The Lithogeochemical Characteristics and Protolith Formation of Khondalite Series in Daqingshan Region, Inner Mongolia;
内蒙古大青山地区孔兹岩系的岩石地球化学特征及原岩建造
5.
The REE Geochemistry of Granitic Rocks in Qingyuan Archean Greenstone-Granite Terrene
清原太古代花岗—绿岩区花岗岩的稀土地球化学
6.
As water journeys down toward the magma( molten rock) under the Earth, it begins to dissolve gold atoms from the nearby rocks.
在水流经地下的岩浆（化的岩石）会从附近的岩石中溶解金原子。
7.
MAJOR AND TRACE ELEMENT GEOCHEMISTRY OF THE ARCHEAN QINGYUAN GRANITE-GREENSTONE TERRANE
清原太古代花岗岩-绿岩地体的常量和微量元素地球化学证据
8.
ON THE PROTOTITH RECONSTRUCTION AND GEOLOGICAL IMPLICATIONS OF EARLY ARCHAEAN METAMORPHIC ROCKS IN EASTERN HEBEI
冀东迁西-迁安地区早太古代变质岩系原岩恢复及其地质意义
9.
The Geophysical Response and Exploration Principle on Litho-Stratigraphic Reservoir
岩性地层油气藏储层地球物理响应与勘探原理
10.
Geochemistry and rock series of quartz monzonite intrusion in west-side of Datong on Qinghai-Xizang Plateau
青藏高原大同西侧石英二长岩体地球化学及岩石系列
11.
Prototype Observations and Theoretical Analysis on Composite Large Diameter Pile Foundation Socketed in Soft Rock;
软岩地基中大直径嵌岩桩复合桩基的原型观测与理论分析
12.
Petrological, Geochemical Compositions and the Origin of the Mesozoic Basalts at the Northeastern Tibetan Plateau
青藏高原东北缘晚中生代玄武岩岩石学地球化学及其成因
13.
Geological features of the northern Fengpingshan gneiss complex and protolith genesis of Weili County,Xinjiang
新疆尉犁县风屏北山片麻杂岩地质特征及原岩成因探讨
14.
A COMPARISON BETWEEN THE AUTOCHTHONOUS AND PARAUTOCHTHONOUS TRANSFORMATION TYPE GRANITOIDS IN EAST QINLING AND SOUTH CHINA CALEDONIAN FOLDBELTS
东秦岭与华南加里东褶皱带原地-准原地改造型花岗岩特征
15.
The diversity index and species richness index of original vegetation in Karst area are lower than in nonkarst area.
石灰岩地区原生植被生物多样性和物种丰富度指数较砂页岩地区的原生植被低。
16.
Rocks and soils, as well as mountains, valleys and plains, differ greatly from place to place.
岩石和土壤，以及山、谷和平原，各地差别很大。
17.
In situ deposits are dark shale with horizontal bedding.
原地沉积为水平层理发育的暗色泥板岩。
18.
Geochemical evidence for original minerology of middle Ordovician limestones
奥陶系中统灰岩原始矿物成分的地球化学证据