amphibolite信息详情
n.[岩]闪岩，角闪岩
amphitropic definition───两性定义
amphipod animal───两足动物
amphictyony definition───矛盾定义
amphioxus olig───文昌鱼
amphipod airflow microstretch belt───双足气流微蚀刻带
amphiuma family───amphiuma家族
amphigory def───两性定义
amphitheater careers───竞技场职业生涯
amphiaster meaning───两旁词义
amphicoelous centrum───两凹椎体
amphibolite facies rocks in the fracture belt have been superimposed by retrograde green-schist facies with neoformation of chlorite.───断裂带中已存在的角闪岩相岩石已与绿泥石新形成的逆行绿片岩相叠加。
first type is residuals of metamorphic rocks of high amphibolite facies.───一类为属于高角闪岩相的变质岩（残余）包体；
host rocks were metamorphosed to the amphibolite and granulite facies.───围岩变质级别达到角闪岩相和麻粒岩相。
Mostly metamorphic facies is amphibolite facies, partial up to granulite facies.───变质相多为角闪岩相，局部达麻粒岩相。
Granulite - the metamorphic gneiss district level are mostly granulite facies to senior amphibolite facies.───麻粒岩-片麻岩区的变质程度多属麻粒岩相到高级角闪岩相。
The result suggests that the protolith of amphibolite in Baoyintu Group was basalt which formed in the island-arc environment.───结果表明，宝音图群中斜长角闪岩原岩为岛弧环境中形成的玄武岩。
As a result, the eclogite was transformed to epidote-bearing amphibolite.───榴辉岩转化成含帘石的斜长角闪岩。
the metamorphic process in the formation of garnet amphibolite along the china - pakistan highway profile , west kunlun orogenic belt───西昆仑造山带中巴公路段石榴角闪岩形成的变质地质过程
U-Pb chronology in zircon of magnetite-amphibolite intrusion from western Shandong and its geological implications───鲁西下常庄磁铁角闪岩岩体中锆石U-Pb年代学及其地质意义
There is a suboutcrop of amphibolite facies TTG gneiss overlain by Neoproterozoic Zhangbaling Group at Nanhuang region in Jiashan, East Anhui.
The pre-exist amphibolite facies rocks in the fracture belt have been superimposed by retrograde green-schist facies with neoformation of chlorite, anthophyllite, sericite and cordierite.
Garnet amphibolites from Beiyuan in southwestern Zhejiang Province are the products of high - amphibolite facies metamorphism.
The host rocks were metamorphosed to the amphibolite and granulite facies.
The main rock types include granulitite, mica schist, epidote-plagioclase amphibolite, itabirite and marble.
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The amphibolite xenoliths were from the upper part of lower crust and the lower part of middle crust, bring up to the shallow area of crust .
The late stage is characterized by recrystallization in a stable enviroument. The metamorphism of low pressure type of low amphibolite facies only occurs on the main boundary planes of the zone.
The amphibolite and basic granulite may be comparable to the world's metamorphic tholeiite.