Based on field evidence,it is inferred that the kersantite pipes near Yanzihe in Dabie mountains are temporally and spacially related to Yanshanian postorogenic intermediate to acidic magmatism.
根据野外地质特征,大别山燕子河云斜煌岩脉是与燕山期后造山中酸性岩浆活动有时空联系的。
The Geological Setting and Petrological Features of the Kersantite Near Yanzihe in Dabie Mountains;
大别山燕子河云斜煌岩的地质背景和岩石学基本特征
Geochemistry of Lamprophyres in the Baimazhai Nickel Deposit, Yunnan Province, China: Implications for Their Origin;
云南白马寨镍矿区煌斑岩地球化学及其成因
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。
Lithogeochemical characteristics of No.5 pipe-like lamprophyre in Ningxiang,Hunan province
湖南宁乡Ⅴ号岩管煌斑岩的岩石地球化学特征
The light of the setting sun suffused the clouds.
夕阳的斜晖染遍了云朵。
A Study on the Features of the Marble and the Dolomite in Song Shu-Jiao Mine
云锡松矿白云岩、大理岩特性的研究
Dazu Stone (Sculptures) Carving is as famous as the Buddhist Carvings at Longmen, Dunhuang and Yungang.
大足石刻与龙门、敦煌和云冈石刻齐名。
THE FEATURES OF LIANHUATANG LEUCITI-TIC ALNOITE IN ANYUAN COUNTY,JIANGXI
江西安远莲花塘白榴黄长煌斑岩特征
A variety of diorite consisting chiefly of feldspar.
斜长岩主要含有长石的各种闪长岩
Carbonate rocks are predominantly composed of intra-clastic dolostone, chert dolostone and sand-bearing dolostone.
碳酸盐岩以内碎屑白云岩、燧石白云儿和含砂白云岩为主。
Study on the Mineralogy and Petrology of Kimberlite and Lamproite from the North Part of Shanxi Province, China;
山西北部金伯利岩钾镁煌斑岩岩石学矿物学研究
dolomitic biomicrite
白云石质生物微晶灰岩
magnesian limestone
白云石, 含镁石灰岩
Viewed from afar, Potala Palace looks lofty, resplendent and majestic.
远远望去，布达拉宫高耸入云，金碧辉煌，巍峨壮观。
taxichnic dolomite
具石灰岩原始结构的白云岩
The rock paintings in Lianyungang, Jiangsu Province, were drawn on brown stones.
连云港的岩画刻在深褐色的岩石上，
an oblique fault is one that strikes obliquely or diagonally to the strike of the adjacent rocks.
斜向断层是指断层走向与围岩走向斜交的断层。
Spacings between anticlinal crests and synclinal troughs in the member tend to be equal in some series of folds.
岩层中的背斜峰和向斜谷之间的距离趋于相等。