青年中文amphibolite的意思
amphibolite中文翻譯：
n.[巖]閃巖，角閃巖
amphitropic definition───兩性定義
amphipod animal───兩足動物
amphictyony definition───矛盾定義
amphioxus olig───文昌魚
amphipod airflow microstretch belt───雙足氣流微蝕刻帶
amphiuma family───amphiuma家族
amphigory def───兩性定義
amphitheater careers───競技場職業生涯
amphiaster meaning───兩旁詞義
amphicoelous centrum───兩凹椎體
amphibolite facies rocks in the fracture belt have been superimposed by retrograde green-schist facies with neoformation of chlorite.───斷裂帶中已存在的角閃巖相巖石已與綠泥石新形成的逆行綠片巖相疊加。
first type is residuals of metamorphic rocks of high amphibolite facies.───一類為屬于高角閃巖相的變質巖（殘余）包體；
host rocks were metamorphosed to the amphibolite and granulite facies.───圍巖變質級別達到角閃巖相和麻粒巖相。
Mostly metamorphic facies is amphibolite facies, partial up to granulite facies.───變質相多為角閃巖相，局部達麻粒巖相。
Granulite - the metamorphic gneiss district level are mostly granulite facies to senior amphibolite facies.───麻粒巖-片麻巖區的變質程度多屬麻粒巖相到高級角閃巖相。
The result suggests that the protolith of amphibolite in Baoyintu Group was basalt which formed in the island-arc environment.───結果表明，寶音圖群中斜長角閃巖原巖為島弧環境中形成的玄武巖。
As a result, the eclogite was transformed to epidote-bearing amphibolite.───榴輝巖轉化成含簾石的斜長角閃巖。
the metamorphic process in the formation of garnet amphibolite along the china - pakistan highway profile , west kunlun orogenic belt───西昆侖造山帶中巴公路段石榴角閃巖形成的變質地質過程
U-Pb chronology in zircon of magnetite-amphibolite intrusion from western Shandong and its geological implications───魯西下常莊磁鐵角閃巖巖體中鋯石U-Pb年代學及其地質意義
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.