Ophiolite相关论文
We present new, geological, metamorphic, geochemical and geochronological data on the East Anatolian-Lesser Caucasus oph......
Cretaceous tectonic evolution of the Neo-Tethys in Central Iran:Evidence from petrology and age of t
The Nain and Ashin ophiolites consist of Mesozoic mélange units that were emplaced in the Late Cretaceous onto the cont......
Slab rollback and microcontinent subduction in the evolution of the Zambales Ophiolite Complex (Phil
New radiolarian ages show that the island arc-related Acoje block of the Zambales Ophiolite Complex is possibly of Late ......
Compositional and geochronological signatures of metamafic dykes from the Sangsang peridotites, Sout
In this study we present new mineral chemistry, whole-rock geochemical and zircon U–Pb geochronological data for 12 met......
Chromitite bodies hosted in peridotites typical of suboceanic mantle (s.l. ophiolitic) are found in the northern and cen......
Petrogenesis and tectonic significance of the early Paleozoic Delenuoer ophiolite in the Central Qil
The newly discovered early Paleozoic Delenuoer ophiolite, in the western margin of the Central Qilian Shan, is composed ......
Fluid inclusions in olivine and orthopyroxene of mantle peridotites from the Yushigou ophiolite can be divided into thre......
Geochemistry and regional distribution of ophiolites and associated volcanics in Mianlüe suture, Qin
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7......
The fragment of Paleo-Tethys ophiolite from central Qiangtang, Tibet: Geochemical evidence of metaba
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7......
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7......
Geology and geochemistry of the Bingdaban ophiolitic mélange in the boundary fault zone on the north
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7......
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7......
新疆北部科克森套地区玄武岩出露于超镁铁质岩体的北侧,与玄武质凝灰岩共生,厚度达50～80 m;玄武岩普遍具有片理化、斑状结构;岩石地......
An Upper Crustal Ophiolite Remnant within the Feather River Ultramafic Belt, California: Tectonomagm
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7......
Ophiolites from the Mianlüe Suture in the Southern Qinling and Their Relationship with the Eastern P
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7......
Petrogenetic Evolution of the Bayan Gol Ophiolite-- Geological Record of an Early Carboniferous &quo
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7......
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7......
SHRIMP Zircon U-Pb Dating of Gabbro and Granite from the Huashan Ophiolite, Qinling Orogenic Belt, C
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7......
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7......
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7......
The wedge shaped Dong Tso ophiolitic block is distributed near the transition point from the western to the middle sub–......
Geochemical Features, Age, and Tectonic Significance of the Kekekete Mafic-ultramafic Rocks, East Ku
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7......
Zircon U-Pb Geochronology and Hf Isotopic Constraints on Petrogenesis of Plagiogranite from the Cuom
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7......
Tectonic Evolution of the Meso-Tethys in the Western Segment of Bangonghu-Nujiang Suture Zone: Insig
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7......
Platinum-group Mineral (PGM) and Base-metal Sulphide (BMS) Inclusions in Chromitites of the Zedang O
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7......
Various combinations of diamond, moissanite, zircon, corundum, rutile and titanitehave been recovered from the Bulqiza c......
Geochemistry and SHRIMP U-Pb Zircon Dating of Mafic Rocks North of Zunhua City, Eastern Hebei, North
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7......
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7......
The Altyn Tagh Mountain is the main area where the Precambrianbasements of Tarim craton are exposed. There are two ophio......
The total PGE amount (∑PGE) of mantle peridotite in the Jiding ophiolite is slightly higher than that of the primitive ......
Based on the theory of plate tectonics, combining with the isotopic dating of ophiolite, igneous and volcanics, geochemi......
Geochronology and Nd and Pb isotope characteristics of gabbro dikes in the Luobusha ophiolite, Tibet
We report a combined internal and whole-rock Sm-Nd isochron age, and Nd and Pb isotopic data for gabbro dikes of the Luo......
Silicon(Si)-rutile separated from the Luobusa podiform chromitite in the Yarlung Zangbo ophiolite of southern Tibet is t......
Ophiolites from the Mianl e Suture in the Southern Qinling and Their Relationship with the Eastern P
The Mianltüe suture extends from Demi-Nanping-Pipasi-Kangxian to the Lüeyang-Mianxian area, then traverses the Bashan ......
Geochemistry and regional distribution of ophiolites and associated volcanics in Mianl e suture, Qin
Systematic studies of the ophiolites and associated volcanics stretching more than 1500 km from the Derni-Nanping-Pipasi......
Petrogenetic Evolution of the Bayan Gol Ophiolite-- Geological Record of an Early Carboniferous “Red
The Bayan Gol ophiolite fragment is a portion of the North Tianshan Early Carboniferous ophiolite belt. This ophiolite b......
Exsolutions of Diopside and Magnetite in Olivine from Mantle Dunite, Luobusa Ophiolite, Tibet, China
The exsolutions of diopside and magnetite occur as intergrowth and orient within olivine from the mantle dunite, Luobusa......
日喀则蛇绿岩位于雅鲁藏布构造带中段,其成因和构造环境仍存在较大争议。日喀则蛇绿岩下部为蛇纹石化地幔橄榄岩,壳幔过渡带缺失超......
蛇绿混杂岩带作为造山带最重要的组成部分之一,其形成和就位过程与区域造山事件密切相关。通过系统梳理北山造山带蛇绿混杂岩的研......
内蒙古北山地区阿民乌素蛇绿岩是芨芨台子-小黄山蛇绿岩带的重要组成部分,主要由变质辉长岩和极少强蛇纹石化橄榄岩组成。变质辉长......
雅鲁藏布江蛇绿岩带内多个地幔橄榄岩体产有金刚石、碳硅石等异常矿物组合,为了进一步探讨这些异常矿物形成的物理化学条件,在前人......
介绍了基于小波变换的反射光谱分析技术的基本理论和方法；运用此技术手段对克拉玛依市白碱滩区西侧地区40条岩石野外光谱曲线数据进......
西准噶尔西缘巴尔鲁克山西南部存在近东西向的也节拜蛇绿混杂岩带，带内基性一超基性岩发育，基性一超基性岩与南北围岩接触带内构造发......
在可可西里地区蛇形沟一带发现的蛇绿岩主要由辉长岩、辉绿岩、玄武岩三种岩石组成，岩石呈段块出露。根据目前已获得的蛇绿岩的同位......
班公湖蛇绿岩带位于班公湖-怒江结合带西段,蛇绿岩均遭受了强烈挤压构造变形而形成蛇绿混杂岩带.通过对不同类型的蛇绿混杂岩片按......
雅鲁藏布江蛇绿岩带是冈瓦纳板块与欧亚板块汇聚的几条主要缝合带之一,路曲蛇绿岩位于雅鲁藏布江蛇绿岩带中部.分析了路曲蛇绿岩中......
蛇绿岩中的辉绿岩岩墙是洋脊扩张的产物，其形成年龄代表了扩张事件的时间，也代表了蛇绿岩的形成时代。对雅鲁藏布江缝合带中段桑桑蛇......
蛇绿岩是造山带研究的关键问题之一,文章在野外地质调查的基础上,通过岩石学、同位素年代学、地球化学等综合研究,认为东秦岭丹凤......
对祁连山西段香毛山组正层型及其周边地区的地质调查和岩石学、地层古生物学研究发现，原划香毛山组并非正常的正式岩石地层单位，而是......
滇东南八布地区发育一套晚古生代超镁铁质-镁铁质杂岩,是认识古特提斯分支洋构造演化的重要窗口,而其中以火山岩为赋矿围岩的杨万......
