1) two phases of ophiolitic mélanges
2期蛇绿混杂岩
2) Ophiolitic mélange
蛇绿混杂岩
1.
Characteristics and tectonic significance of the Solon Mountain ophiolitic mélange in the Mandula area, Darhan Muminggan, Inner Mongolia;
内蒙古达尔罕茂明安联合旗满都拉地区索伦山蛇绿混杂岩的特征及构造意义
2.
Composition and geochemistry of the Subashi ophiolitic mélange in the West Kunlun and its geological significance;
西昆仑于田南部苏巴什蛇绿混杂岩的组成、地球化学特征及地质意义
3.
The Shiquan River ophiolitic mélange zone in Xizang: The delineation and significance of a new archipelagic are-basin system;
西藏狮泉河蛇绿混杂岩带——一个新的多岛弧盆系统的厘定及意义
3) ophiolitic melange
蛇绿混杂岩
1.
Discovery and significance of ophiolitic melanges at Diancang Mountain in northwestern Yunnan;
滇西北点苍山蛇绿混杂岩的发现及意义
2.
Situated in the western segment of the Bangong-Nujiang junction zone,Bangong Lake ophiolitic melange belt is the relics of subductional collision and extinction of the Mid-Tethyan Ocean.
班公湖蛇绿混杂岩带位于班公湖-怒江结合带西段,是中生代特提斯洋消亡的遗迹。
3.
This paper reports the Sm-Nd and Rb-Sr isotopic chronology of the main melange blocks and the MORB volcanic rocks from the Yangjiapeng area and the IAT volcanic rocks from the Xiaofu area, which comprise the ophiolitic melange of Huashan.
对湖北省随州地区组成花山蛇绿混杂岩的杨家棚MORB型火山岩、小阜岛弧型火山岩进行了Sm-Nd、Rb-Sr同位素分析。
4) ophiolite complex
蛇绿混杂岩
1.
The original rock of meta-basic rocks in ophiolite complex of Wandashan orogenic belt can be divided into two sorts.
完达山造山带蛇绿混杂岩中变质基性岩原岩主要有两种类型:在大顶子山和仙人台附近蛇绿岩带中的变质玄武岩地球化学具有T iO2含量偏高,高场强元素N b,T a,Z r,H f等富集,大离子亲石元素R b,Sr,B a等相对富集;LREE富集,体现出洋岛型玄武岩的特征。
2.
In this paper the Yaluzangbu suture zone is divided into 6 structural zones, and the ophiolite complex can be further divided into 4 secondary rock slices.
构造岩片作为造山带中非史密斯地层地区的填图单位有其重要的地质意义,本文将雅鲁藏布江缝合带分为6大构造岩片,其中蛇绿混杂岩岩片又分4个次级岩片,进一步阐述了缝合带内不同单元具有不同岩性和不同构造型式,是一条复杂的构造带,并发现俯冲板块一侧的不同构造单元具有自南而北,由脆性变形到低温高压变质、脆-韧性变形,超基性岩的深层次韧性变形的分布规律,大多数岩片的分布是通过多重逆冲推覆型或走滑型的断层将其从地壳深部挤出定位的。
5) ophiolite melange
蛇绿混杂岩
1.
Geochemical evidence of MORB and OIB combination in Hongliugou ophiolite melanges, Altun fault belt;
阿尔金红柳沟蛇绿混杂岩中MORB与OIB组合的地球化学证据
2.
The different views on the age, lithofacies and contact relationship of the strata related to the ophiolite melange belt in northeastern Jiangxi Province lead to the different explanations on the history of geological evolution of South China.
对赣东北蛇绿混杂岩带相关地层的时代、沉积相和接触关系等方面认识的重大分歧 ,导致对华南地质演化史的不同解释。
3.
Comprehensive studies of geology,petrochemistry,geochemistry and isotopic chronology revealed that the ophiolite melange in Hongliuhe area consists of peridotite,gabbro,basalt and back arc volcanic and sedimentary rocks.
地质、岩石化学、地球化学、同位素年代学综合研究证明 ,红柳河地区蛇绿混杂岩由橄榄岩、辉长岩、玄武岩和弧后火山 -沉积岩系组成。
6) ophiolite
[英]['ɔfiəlait,'əufiəlait] [美]['ɑfiə,laɪt, 'ofi-]
蛇绿混杂岩
1.
Discovery of the Qimanyute ophiolite in the West Kunlun and its geological significance;
西昆仑其曼于特蛇绿混杂岩的发现及其地质意义
补充资料：混杂岩
| 混杂岩 melange 受板块构造作用而变形并能在地质图上填绘出的特殊岩石体。又称混杂堆积。由外来岩块、原地岩块、基质三部分组成。外来岩块主要来自俯冲板块上的放射虫硅质岩、枕状熔岩和归属于洋壳和地幔物质的基性、超基性岩碎块，有时还有海沟内壁上的蓝片岩；基质一般是相对塑性的泥、砂质岩石。所有上述各岩石碎块大小不等，形状各异彼此以构造关系相接触，且均经受了不同规模的剪切作用；它们与俯冲带大致平行的带状分布于特定的构造部位，带宽数十至数百千米，延伸可达数千千米，带内柔性褶皱和叠瓦状推覆构造发育。由于外来岩块以蛇绿岩套的各组分岩石为主，故也称蛇绿混杂岩，是鉴别古海沟的重要标志。板块构造学认为混杂岩是构造活动与沉积作用的综合产物。美国西海岸圣弗兰西斯科混杂堆积是一套典型的混杂岩。中国喜马拉雅山、天山、西秦岭等地也相继发现了蛇绿混杂岩。 |
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条