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1)  high-pressure quartzo-feldspathic granulite
长英质高压麻粒岩
1.
A study on geochemical character of high-pressure quartzo-feldspathic granulite in Songshugou area, east Qinling, shows that its protolith is composed mainly of graywacke or arkose, and a little of subalkaline acid volcanic rock or magmatic rock with characteristies of mantle source.
地球化学特征研究表明,东秦岭松树沟长英质高压麻粒岩的原岩性质主体为杂砂岩或长石砂岩,少量为亚碱性的酸性火山岩或岩浆岩并具慢源成因;其古构造环境类似于活动大陆边缘。
2)  felsic granulite
长英质麻粒岩
1.
Geochronology and geodynamic implications of the felsic granulite xenoliths from the Hannuoba Basalt;
汉诺坝长英质麻粒岩包体同位素年代学及其地球动力学意义
2.
A felsic granulite from South Neimenggu(Inner Mongolia) of China has been deformed at the confining pressure of 1100 MPa, temperatures of 650~900℃, and strain rates of 10 -4 ~10 -7 s -1 .
在温度为650~900℃、围压为1100ΜΡa和应变率为10-4~10-7s-1的条件下,对大陆下地壳组成中的一类重要岩石——长英质麻粒岩进行了流变实验。
3.
LA-ICPMS U-Pb dating was conducted on three textural domains in zircon from a high-temperature high-pressure felsic granulite in the Huangtuling area, North Dabieshan, Central China.
本研究应用激光剥蚀技术测定了北大别黄土岭高温-高压长英质麻粒岩锆石3个结构域的UPb年龄。
3)  leptite ['leptait]
长英麻粒岩
4)  high-pressure granulite
高压麻粒岩
1.
Zircon SHRIMP U-Pb age of the Paleoproterozoic high-pressure granulites from the Sanggan area,the North China Craton and its geologic implications;
华北克拉通桑干地区高压麻粒岩的锆石SHRIMP U-Pb年龄及其地质含义
2.
The Zhibai Formation Complex high2ressure granulites within the Eastern Himalayan syntaxis are a succession of high-pressure granulites as the youngest granulites in the world formed at the lower crustal root zones.
东喜马拉雅构造结一带断续分布的直白高压麻粒岩,是一套相当于下地壳根带深度形成的高压麻粒岩相岩石。
3.
The Hengshan Neoarchean high-pressure granulite terrain is one of the best preserved high-pressure granulite regions in the central North China Block (NCB).
恒山中段高压麻粒岩区是华北克拉通新太古代高压麻粒岩最好的露头区之一,北部为强烈重熔的灰色片麻岩区,构造样式以穹窿、近水平韧性剪切带为主,中部以近东西向的右旋走滑剪切带与南部变形变质程度相对较低的岩石单元相接,后者主要的岩石类型为均匀的英云闪长质片麻岩和变质辉绿岩墙。
5)  High pressure granulite
高压麻粒岩
1.
High pressure granulites are extensively developed in the Jianping complex, western Liaoning province.
辽西建平杂岩中广泛发育高压麻粒岩块体 ,其特征为在基性岩中出现石榴石 +单斜辉石 +斜长石 +石英±角闪石 ,利用 TWQ方法结合传统地质温压计估算其变质条件为 T=785~ 82 0℃ ,P=1。
2.
This paper presents the detailed studies of Ti rich amphiboles from high pressure granulites in southern Henan Province by means of optical analysis,electron microprobe analysis,infrared absorption spectrometry and single crystal X ray diffraction.
作者用光学方法、电子探针分析方法、红外吸收光谱方法和 X射线粉晶衍射方法对豫南高压麻粒岩中的富钛角闪石类进行了详细研究。
3.
Between the Chongli arc type greenstone belt and the Huai an ancient continent block, there develops a consecutive platy high pressure granulite belt.
在崇礼岛弧型绿岩带与怀安古陆块之间,从怀安大虎沟,经宣化大东沟至赤城沤麻坑发育一条大体呈东西走向并向南倾斜的板状高压麻粒岩带。
6)  high pressure mafic granulites
高压镁铁质麻粒岩
1.
Recently,a high pressure mafic granulites block has discovered along the northern borderland of the Tongbai Dabie orogenic belt.
位于桐柏大别山造山带北缘桐柏信阳地段的豫南高压镁铁质麻粒岩块体主要由石榴角闪二辉麻粒岩类组成。
补充资料:麻粒
分子式:
CAS号:

性质:猪皮反绒革的一种缺陷。表现为皮革肉面绒毛不够紧密或几乎不起绒,显露毛囊突出的小点,手摸有糙手的硬刺感,甚至留有残毛根。

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