1) amphibolite facies
角闪岩相
1.
Petrogenesis of amphibolite facies garnet clinopyroxenite from the Mama valley,Cona area,southeastern Tibet;
藏东南错那县麻玛沟角闪岩相石榴辉石岩成因研究
2.
Based on the study of petrography and mineralogy, the enclaves in granitoids are parametamorphites of amphibolite facies and granulite facies, and the types of enclave rocks include hyperthene-granulite, geneiss, granulite and enclaves riched mica.
据包体岩相学及矿物学研究 ,包体岩石为角闪岩相到麻粒岩相的副变质岩 ,岩石类型有麻粒岩、变粒岩、片麻岩和富云包体。
2) lower amphibolite facies
低角闪岩相
3) upper amphibolite facies
高角闪岩相
1.
Thermobarometry suggests that the peak metamorphism of the rocks reached upper amphibolite facies conditions of 560-670 ℃ and 0.
变质作用温压估算结果显示,这些包体的峰期变质条件达到了高角闪岩相,其T=560~670℃,p=0。
4) amphibolite facies deformation
角闪岩相变形
5) epidote-amphibolite facies
绿帘石角闪岩相
6) green schist-lower amphibolite facies
绿片岩-低角闪岩相
1.
Fe isotope fractionation between magnetite and pyrite during green schist-lower amphibolite facies metamorphism;
绿片岩-低角闪岩相变质条件下磁铁矿与黄铁矿间的Fe同位素分馏
补充资料：斜长角闪岩
| 斜长角闪岩 amphibolite 由区域变质作用形成的一种变质岩。主要由普通角闪石和斜长石组成（两者含量大体相等），可含少量黑云母、石英、铁铝榴石、绿帘石等。具粒状、柱状变晶结构，片状，片麻状构造。可根据构造＋特征矿物＋基本名称的原则命名，如条带状石榴子石斜 长角闪岩、芝麻 点榴辉斜长角闪岩等。通常认为它形成于高绿片岩相（绿帘角闪岩相）至角闪岩相的变质条件，有时也可形成于接触变质作用。在老变质岩地区广泛发育。 |
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