Royal Mmhogany

Mineralogical Characteristics of Cordierites in Krn Hy Crd Granulites from the Larsemann Hills, East Antarctica

东南极拉斯曼丘陵柱晶紫苏堇青麻粒岩中堇青石的矿物学特征

THE CORDIERITE-SILLIMANITE ASSEMBLAGE IN THE ARCHAEAN GRANULITE BELT ON NORTH CHINA PLATFORM AS AN INDICATOR FOR LOWPRESSURE GRANULITE FACIES

华北地台太古代麻粒岩相带的堇青石-夕线石组合:低压麻粒岩相的标志

THE MINERALOGICAL CHARACTERISTICS OF HEXAGONAL PYRAMID BERYL FOR DACALASU GRANITE-PEGMATITE IN ALTAY,XINJIANG

新疆大卡拉苏花岗伟晶岩锥状绿柱石矿物特征

Study of the Corderiate Based Mg-Al-Si Glass Ceramics;

Mg-Al-Si系堇青石基微晶玻璃的研究

Characteristics and Temperature-Pressure Conditions for Crystallization of Pyroxene in Archean Granulite Facies of Inner Mongolia

内蒙古太古宙麻粒岩相岩石中辉石特征和结晶温压条件

Study on preparation of ordered porous cordierite with colloidal crystals template

胶体晶体模板法制备有序多孔堇青石材料研究

Isotopic Chronological Restriction of Granulite Facies Metamorphism in Daqingshan Area, Inner Mongolia;

内蒙古大青山地区麻粒岩系变质作用的同位素年代学制约

blastoporphyritic leptite

变余斑状长英麻粒岩

THE DISCOVERY OF GRANULITES AND GRANULITE FACIES IN THE XIAOLINZI IRON DEPOSIT,ANSHAN,NORTHEAST CHINA

鞍山小岭子铁矿麻粒岩及麻粒岩相的发现

Research of Crystallization and Properties on the Cordierite Based MAS Glass-ceramics;

MAS系统堇青石基微晶玻璃的晶化行为和性能研究

Study on Abrasion Resistance of the Columnar Grain Zone in High Cr Cast Iron

铸态高铬铸铁柱状晶粒区耐磨性研究

A dichroic violet-blue to gray mineral silicate of magnesium, aluminum, and sometimes iron.

堇青石一种呈介于紫蓝于灰色的二色性矿物，是含镁、铝、有的也含铁的硅酸盐

a granular crystalline intrusive rock.

一种由小粒形成的晶体侵入岩。

cordierite whiteware

堇青石白坯陶瓷制品

Retrogressive textures and metamorphic reaction features of Al-rich gneisses in the granulite facies belt from northwestern Hebei province

冀西北麻粒岩相带富铝片麻岩的退变结构及其变质反应性质

CONTRASTING ARCHAEAN GRANULITE FACIES ROCKS FROM EASTERN HEBEI, NORTH CHINA

冀东太古代高级变质地体中两类麻粒岩相深成片麻岩

Examples are soybean, rapeseed and tlaxseed, wheat germ, hempseed, and perilla oils, with soybean being the most important.

例如大豆、油菜籽和亚麻籽、小麦胚、大麻子和紫苏子油。

The amphibolite and basic granulite may be comparable to the world's metamorphic tholeiite.

斜长角闪岩和基性麻粒岩可与世界变质拉斑玄武岩对比.