1.
Tectonic Characteristics and Evolution of the Yagan Metamorphic Core Complex;
亚干变质核杂岩的地质构造特征及其演化
2.
The Tectono-magmatic Interactions of Liaonan Metamorphic Core Complex;
辽南变质核杂岩晚中生代构造岩浆关系
3.
Deformation Characteristics of Middle Ductile Rheological Bed of the Yiwulüshan Metamorphic Core Complex in Western Liaoning Province
辽西医巫闾山变质核杂岩中间流变层变形特征
4.
CHARACTERISTICS OF FANGSHAN METAMORPHIC CORE COMPLEX,BEIJING AND A DISCUSSION ABOUT ITS ORIGIN
北京房山变质核杂岩的基本特征及其成因探讨
5.
Liaonan-Wanfu Metamorphic Core Complexes and Their Regional Tectonic Implication;
辽南—万福变质核杂岩及其区域构造意义
6.
lithic subarkosic wacke
岩屑亚长石砂岩质杂砂岩
7.
GEOTECTONIC FEATURES OF THE COMPLEX IN THE METAMORPHOSED CORE OF THE NALATI TECTONIC ZONE IN WESTERN TIANSHAN,SINKIANG
新疆西天山那拉提构造带变质核部杂岩地质构造特征
8.
Structural Characteristics and Geological Signifcance of the Jiaoziding Metamorphic Core Complex at the Northwest Margins;
扬子地块西北缘轿子顶变质核杂岩构造特征及其地质意义
9.
Results The tectonic characteristics and evolution of the Xiaoqinling area do not fit those of typical MCC.
结果小秦岭地区的构造特征与变质核杂岩特征不符。
10.
Primary Research on Geochemistry and Geochronology of the Laojunshan Metamorphic Core Complex, Southeastern Yunnan;
滇东南老君山变质核杂岩地球化学和年代学初步研究
11.
Zircon SHRIMP U-Pb age of Yinmawanshan and Zhaofang pluton in South Liaoning metamorphic core complex and its geological implications.
辽南变质核杂岩饮马湾山和赵房岩体锆石SHRIMP U-Pb年龄及其地质意义
12.
Metamorphism of Indosinian Metamorphic Enclaves in the Tongbai Complex,Central China
桐柏杂岩中印支期变质岩包体的变质作用
13.
Gold mineralization of these two deposits occurs within the Archean metamophic rocks of Sanggan Group and Hercynian alkaline complex , respectively.
小营盘金矿产于太古宇桑干群变质岩中，东坪金矿产于海西期碱性杂岩体中。
14.
lithic arkosic wacke
岩屑长石砂岩质杂砂岩
15.
prehnite-pumpellyite-metagreywacke facies
葡萄石-绿纤石-变质杂砂岩相
16.
Evolution of Metamorphism of Archean Jianping Metamorphic Complex from the Western Liaoning Province
辽西太古代“建平变质杂岩”的变质作用演化
17.
Metamorphism of Al Rich Gneisses in Taihang Mountain Archean Metamorphic Complex
太行山太古宙变质杂岩中富铝片麻岩的变质作用
18.
The supracrustal sequences in the Dabie complex in northeastern Hubei belongs to a late Archean stratified metamorphic sequences.
鄂东北大别杂岩中的表壳岩系属于晚太古代层状变质岩系。