- 角閃巖相
- 閃巖相
- amphibolite: n. 【礦物】閃巖。
- facies: n. 〔pl.〕 〔單復(fù)同〕 1.顏面，外觀；外表。 2 ...
- albite-epidote-amphibolite facies: 鈉長(zhǎng)簾閃巖相
- albiteepidote amphibolite facies: 鈉長(zhǎng)石綠簾石角閃巖相
- alpine amphibolite facies: 阿爾卑斯角閃巖相
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amphibolite facies中文什么意思
- 角閃巖相
- 閃巖相
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例句與用法
- Albite - epidote - amphibolite facies
鈉長(zhǎng)簾閃巖相 - Lots of information suggest that the metamorphism process of this area are from granulite facies to amphibolite facies and the retrograded metamorphic path is basically a cw nearly isothermal decompressional evolvement trend
各種信息表明本區(qū)的變質(zhì)作用是由麻粒巖相退變到角閃巖相。退變質(zhì)軌跡基本上是一個(gè)順時(shí)針近等溫減壓型演化趨勢(shì)。 - All these rocks aforementioned are mainly parametamorphic rocks . milan , kaqiang and alamasi group underwent high - grade metamorphism of amphibolite facies , together with weak migmatism . they share the same geochemistry and total ree and many other chracters
二者主要為副變質(zhì)巖石，米蘭巖群和卡羌巖群、阿拉瑪斯巖群變質(zhì)較深為角閃巖相，普遍弱混合巖化，它們具有非常相似的地球化學(xué)特征，稀土元素總量及其它特點(diǎn)一致或相近。 - Detail mapping shows that the yagan mcc consists of crystallized metamorphic core ( low plate ) , detachment zone and upper plate . the metamorphic core consists of can be further subdivided into two level parts low - level high metamorphic and upper - level shallow metamorphic structural slice and between them there exists a ductile shear zone . thus the whole texture of the mcc is characterized by " three layers and tow zones " this reveals a process of extensional uplift of poly - level slices by poly ductile shear zones , a characteristics of poly - level extensional structural systems . the deformational environments change vertically in a sequence of high amphibolite facies
亞干變質(zhì)核雜巖由下盤(pán)結(jié)晶巖系變質(zhì)核、拆離帶和上盤(pán)巖系構(gòu)成，其中，變質(zhì)核由四個(gè)單位及許多花崗巖體(脈)組成，可進(jìn)一步分為中深和中淺變質(zhì)兩個(gè)構(gòu)造單位(巖片) ，之間發(fā)育次級(jí)韌性拆離帶(花崗質(zhì)糜棱巖帶) ，加上上盤(pán)總體構(gòu)成“三層兩帶”的結(jié)構(gòu)特點(diǎn)。