mélange相关论文
The Pre-Jurassic Ophiolitic M(E)Lange in the Northern Margin of North China Craton: Geochemical Char
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A Geological Section of the Jurassic Mugagangri Group in Gaize, Tibet, and Its Implications to the E
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Lower Cretaceous turbidites in the Shiquanhe–Namco Ophiolite Mélange Zone, Asa area, Tibet: Constrai
Turbidites fromthe Shiquanhe–Namco OphioliteMélange Zone(SNMZ)record critical information about the tectonic affinity ......
The study of terranes has already become an important subject in research of the Circum-Pacific continental margin. This......
New paleontological evidence suggests that the composition of the matrix and slices from the middle and the south of the......
The subduction channel is defined as a relatively thin and weak zone with coherent kinematics between the descending and......
本文通过对荣华二采区10...
帮果目—波库蛇绿岩带位于雅鲁藏布江缝合带的最西段，由帮果日蛇绿岩和波库混杂岩构成，呈北西展布，长128km，宽5～10km。帮果日蛇绿岩由方......
羊卓绒错混杂岩是一条长达2000 km的构造破碎岩带,出露于西藏南部雅鲁藏布江缝合带以南.该缝合带于新生代欧亚碰撞后闭合,记录了特......
从构造角度将西天山分为北天山弧前混杂岩带、中天山复合岩浆弧带、南天山弧后混杂岩带及南天山南缘晚古生代岩浆弧带；并且重建其古......
在甘孜－理塘断裂带北段首次应用构造岩片观点按构造－建造组合特征将甘孜－理塘断裂带北段划分为４个具岩性组合特征、构造意义的构造岩片......
ＩＮＴＲＯＤＵＣＴＩＯＮＴｈｅＮｏｒｔｈｅａｓｔＣｈｉｎａａｎｄｉｔｓａｄｊａｃｅｎｔｒｅｇｉｏｎｐｒｅｓｅｎｔａｕｎｉｑｕｅｔｅｃｔｏｎｉｃｐａｔｅｒｎ，ｗｈｉｃｈｉｓｄｉｓｔｉｎｇｕｉｓｈｅｄｂｙｌａｒｇｅｓｃａｌｅＮＥｔｒｅｎｄｉｎｇｇｒａｎｉ.........
通过乌苏里地区中苏合作对比研究，对该区的构造有了以下一些新的认识：若干地体的拼贴奠定了东北亚大陆边缘的构造格局，地体的拼贴在时......
分布于昆秦接合部－苦海－赛什塘构造混杂带中的混杂岩，经历了中高压绿片岩相变质和同期强烈的生剪切变形，经推算其变质条件P＝0.5-0.7GPa,......
摩天岭褶皱带位于扬子地台西北缘,主要由中、晚元古宇“碧口群”火山、沉积杂岩系组成。笔者认为:该套杂岩系在刘家坪—铜钱韧性剪......
Yamdrok melange occurs south of, and parallel to, the Yarlung—Zangbo ophiolites, extending several hundreds of kilometr......
Jinshajiang melange belt locates between Jianda|Weixi island arc and Zhongzha massif. The melange belt and island arc ma......
以湖南马底驿地区１：５万区调和专题研究资料为基础，指出板溪群岩石（包括其下伏的冷家溪群）不是构造杂岩，而是前震旦系正常的地层序列，江南古......
The relationships and boundary between the North China and Tarim plates have been unclear for a long time ; however, the......
Lichi melange,located in the southern coastal range,eastern Taiwan,China,is a typical tectonic melange of the plate'......
