1) dehydration-melting in amphibolite
斜长角闪岩脱水熔融
1.
Textural development of dehydration-melting in amphibolite at 1.0-3.5 GPa and 950 ℃—Effect of pressure and time
950℃、1.0～3.5GPa下斜长角闪岩脱水熔融——压力和时间对结构的影响
2) amphibolites
斜长角闪岩
1.
Petrology and geochemical characteristics of amphibolites in Yangtizishan-Moshishan anatase ore deposit,Inner Mongolia;
内蒙古羊蹄子山-磨石山锐钛矿矿床斜长角闪岩类的岩石学和地球化学特征
2.
Amphibolites from HP/UHP metamorphic belt in the North Qaidam Mountains can be subdivided into two types.
分布在柴北缘超高压变质带中的斜长角闪岩主要有两种类型,一种由榴辉岩退变而成,一种只经历角闪岩相变质作用。
3.
This study of the geochemical characteristics of the amphibolites from the Dabie core complex is important for tracing the origin of the Dabie core complex unit.
大别核部杂岩单元中斜长角闪岩的地球化学特征对于认识大别核部杂岩单元的特征及归属有着十分重要的意义。
3) amphibolite
[英][æm'fibɔ,lait] [美][æm'fɪbə,laɪt]
斜长角闪岩
1.
SHRIMP U-Pb dating of zircons from amphibolite in the main hole of the Chinese Continental Scientific Drilling Project;
中国大陆科学钻探工程主孔斜长角闪岩中锆石的SHRIMP U-Pb定年及其地质意义
2.
Chronology of amphibolite protolith in Haicheng of southern Liaoning:evidence from LA-ICP-MS zircon U-Pb dating;
辽南海城斜长角闪岩原岩的形成时代:锆石LA-ICP-MS U-Pb定年证据
3.
Geochemistry and Geochronology of Amphibolite from the Hongliugou Area,Altyn Tagn,Northwestern China;
阿尔金红柳沟斜长角闪岩的形成时代及其地球化学特征
4) two-pyroxene amphibolite
二辉斜长角闪岩
5) pyroxeneferous amphibolites
含辉石斜长角闪岩
1.
In this research, pyroxeneferous amphibolites of the lower Fuping Group complex show an Sm-Nd isochronal age of 3352±50 Ma and an average model age of 3374 Ma, which indicates that th.
本次对阜平岩群下部含辉石斜长角闪岩Sm-Nd同位素年代学的详细研究,获得Sm-Nd等时线年龄3352±50Ma和平均模式年龄3374。
6) dehydration melting
脱水熔融
1.
A number of experimental studies on the dehydration melting of metabasalt show that the key factors controlling the composition of adakitic rocks are starting materials, water contents, and thermal structure (p-T paths) of lithosphere.
大量变玄武岩脱水熔融实验表明,制约埃达克岩形成的主要因素是源岩、水和地壳热结构(p-T轨迹)。
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