1.
classification of in-situ rock
原地岩石的鉴定分级
2.
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
3.
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。
4.
The rocky crust of the earth.
岩石圈地球的岩石外表
5.
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
6.
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
7.
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。
8.
NEW METHOD OF CALCULATION OF PROJECTILE PENETRATION INTO ROCK
钻地弹侵彻岩石深度计算新原理与方法
9.
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
10.
Sedimentary significance of the autochthonous glauconite in stromatolitic limestones of the Mesoproterozoic Tieling Formation in Jixian,Tianjin,North China
天津蓟县中元古界铁岭组叠层石灰岩中原地海绿石的沉积学意义
11.
The actual cause of the quake itself is the rupturing or breaking of rocks at or below the earth's surface.
地震本身的真正原因是地球表面的或地底下的岩石断裂或破裂。
12.
Lithostratigraphy,Biostratigraphy and Climatic Stratigraphy in the North China Plain since Late Pleistocene
华北平原晚更新世以来岩石地层、生物地层及气候地层
13.
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。
14.
Mineral Chemistry of Peridotitic Xenoliths in Yangyuan Cenozoic Basalts: Significance for Lithospheric Mantle Evolution Beneath the Trans-North China Orogen
河北阳原新生代玄武岩中橄榄岩捕虏体矿物化学特征：华北内部山带岩石圈地幔演化意义
15.
Mineral Chemistry of Peridotite Xenoliths in Yangyuan Cenozoic Basalts:Significance for Lithospheric Mantle Evolution beneath the North China Craton
河北阳原新生代玄武岩中橄榄岩捕虏体矿物化学:华北岩石圈地幔演化
16.
Petrogenesis of two kinds of Cenozoic ultrapotassic volcanic rocks in Qinghai-Tibet Plateau:Constraints from experimental petrology and geochemistry
青藏高原新生代两类超钾质岩石的成因——实验岩石学和地球化学约束
17.
What is known as the Yunnan-Guizhou Plateau is a region dominated by limestone formations, higher at the western end and dropping gradually in the three other directions.
云贵高原为石灰岩地区，且地势由西向东、北、南三处倾斜。
18.
Petrographical and geochemical characteristics of the Cretaceous granitoids in the Tianshuihai area,western Qinghai-Tibet Plateau,China and its geological significance
青藏高原西部甜水海地区白垩纪花岗岩类的岩石学 地球化学特征及其地质意义