韧性剪切带叠加在在构造混杂岩带上。
The ductile shear zone is superimposed on the tectonic melange zone.
同时指出，沉积混杂岩是研究隐伏基底的重要窗口。
Meanwhile, they point out that the sedimentary melange is an important window to study the concealed basement.
初步总结了西金乌兰蛇绿构造混杂岩带的演化过程。
Confined the Xijir Ulan tectonic melange belt consists of a sierise blocks seprated by thrust towards south.
蛇绿混杂岩破碎混合作用记录了一种递进变形的应变历史。
The disrupting and mingling of the melange may record a strain history of progressive deformation.
该蛇绿混杂岩带是义敦碰撞造山带大地构造相中的弧前混杂带相。
The ophiolite melange zone represents forearc melange facies of the Yidun collision orogens.
威海—乳山麻粒岩带是苏北—胶南构造混杂岩带北东段的北西边缘带。
The Weihai Rushan granulite belt is the northwestern marginal zone of the northeastern section of the Subei Jiaonan tectonic melange zone.
重点论述了甘孜地区三条构造混杂岩带的物质组成、变形特征和形成机制。
Composition, deformation and genetic mechanism of three tectonic melange zones in Garze area are discussed.
干邑里面是数百种罕见的生命之水的争夺，混杂岩年龄为25-130年之间。
The cognac inside is a mèlange of hundreds of rare eaux-de-vies, aged for between 25-130 years.
提出当前用古生物法确定蛇绿岩套形成时代及蛇绿混杂岩定位时代应注意的问题。
They point out the age of ophiolite suite by paleontological method and the emplacement age of ophiolitic melange.
干沟-米什沟蛇绿混杂岩带的变形运动学与科克苏高压变质岩带变形特征完全一致。
The kinematics of Gangou ophiolitic mélange is consistent with that of Kekesu HP metamorphic rocks.
对甘孜-理塘结合带甘孜地区的沉积混杂、火山混杂、构造混杂岩作了系统分析研究。
Sedimentary, volcanic and tectonic me'langes in Garze area in the Garbs-Litang junction are systematically analyzed.
新疆东准噶尔卡拉麦里蛇绿混杂岩的岩石组合为变质橄榄岩、辉长岩、辉绿岩和基性熔岩等。
The Karamaili ophiolite complex in East Junggar of Xinjiang province was composed of metamorphic peridotite, gabbro, diabase and basic lava.
西金乌兰构造混杂岩带为西金乌兰-金沙江缝合带的西端，由于以往研究程度低而认识较为模糊。
The Xijir Ulan tectonic melange belt is the western part of Xijr Ulan-Jinshajiang sutural zone, because study in low degree in the past, it is still indefinite.
新发现的克拉玛依蛇绿混杂岩带分布于准噶尔盆地西北缘，表现为组分齐全的蛇绿岩和增生杂岩。
The newly discovered Karamay ophiolitic mélange distributed along the NW edge of the Junggar basin has a complete sequence of ophiolite and accretionary complex.
依据地层组成结合岩石化学研究，在“构造混杂岩”基础上建立了“双列岛弧”的“沟弧盆体系”模式。
According to stratigraphic compositionand lithochemistry, a"trench-arc-basin system" model for the dual-arrangedisland arc is established on the basis of the "tectonic melange".
运用大陆造山带构造岩片填图方法，首次对九寨沟塔藏构造带进行了系统研究，认为塔藏构造带为一构造混杂岩带。
By using the method of tectonic slab mapping in the continental orogenic belt, the authors carried out a systematic study of the Tazang tectonic belt of Jiuzhaigou.
岩体以小岩株、岩脉及构造岩片产出，普遍受后期构造作用，多数以构造片岩卷入海西期苦海-赛什塘构造混杂岩带内。
The intrusive bodies are output in stocks, dikes and tectonic slices, which were suffered from later tectonism and evolved in the Kuhai-Saishitang Hercynian mélange belt as tectonic slices.
石炭纪牛井山蛇绿混杂岩出露于云南省西南部双江县牛井山—耿马县勐永一带，勐永以北与铜厂街地区的蛇绿混杂岩相接。
Carboniferous Nujinshan ophiolite melange is situated from Nujinshan to Mengyong area, where is dominated by Shuangjiang County and Gengma County respectively, southwestern Yunnan Province.
仁布蛇绿构造混杂带位于雅鲁藏布江缝合带中段之最东部，其间混杂伴生有大量较为新鲜的辉绿岩构造岩块。
The Renbu ophiolitic mélange zone locates in the easternmost middle section of the Yarlung Zangbo suture zone, and there are lots of fresh diabase tectonic block outcrops in the mélange zone.
笔者讨论了其术语、岩块、基质特征、形成机制和古地理古构造条件，并列表分析了它与混杂堆积的区别。
The relevant terminology, block and matrix characteristics, genetic mechanism, palaeogeography and tectonics are discussed in this paper together with their distinction from melanges.
西昆仑赛力亚克混杂堆积由形态、颜色和大小各异的沉积岩块体以及黑色泥质粉砂岩夹灰紫绿色钙质页岩、泥灰岩和层凝灰岩的基质组成。
The Saliyak melange consists of dark-gray to black muddy and silty microclastic rock with intercalation of grayish purple and grayish green calcareous and muddy shale, marl and tuff.
接触变质带可进一步划分为岩焦混杂带、天然焦带、焦化煤带、正常煤带。
The contact metamorphic zone may be further divided into coking coal mixing zone, natural coke zone, coking coal zone and normal coal zone.
岩石学和地球化学特征揭示包体寄主岩为碧玄岩，岩浆没有经历明显分异和同化混杂作用。
Their petrological and geochemical characters suggest that the host rock of the xenoliths is basanite, and the magma has not experienced obvious differentiation and assimilatory contamination.
岩石学和地球化学特征揭示包体寄主岩为碧玄岩，岩浆没有经历明显分异和同化混杂作用。
Their petrological and geochemical characters suggest that the host rock of the xenoliths is basanite, and the magma has not experienced obvious differentiation and assimilatory contamination.
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