1) UHP metamorphic GBPs
超高压变质石榴石橄榄岩
2) Garnet peridotite
石榴橄榄岩
1.
From garnet peridotite to garnert-fre.
对样品进行主量元素、微量元素、稀土元素和Sr、Nd、O同位素分析表明,随着样品MgO含量的增高,Al_2O_3、CaO逐渐降低,呈良好的相关关系,并且大致上从石榴橄榄岩类到不含石榴子石的橄榄岩类主量元素的亏损程度增高,两者一般均比原始地幔主量元素亏损。
3) garnet peridotite
石榴石橄榄岩
1.
The ultramafic rocks in the CCSD-PP3 (China Continental Scientific Drilling) drill-hole consist of dunite and garnet peridotite with a gradual margin between them.
PP3超镁铁岩主要岩石类型有纯橄岩和石榴石橄榄岩,两者为渐变,主要矿物为橄榄石、铬尖晶石、石榴石、单斜辉石和斜方辉石。
2.
It consists of interlayered garnet peridotite and garnet-free peridotite, which have many common compositional features and formed under the same p-T conditions.
岩体由交替出现的石榴石橄榄岩和不含石榴石橄榄岩层组成。
3.
The mineral exsolution in olivine of garnet peridotite from the Sulu area, China and the Arami area, Switzerland, were studied by map analysis in eletronic probe microanalysis(EPMA).
以中国苏鲁石榴石橄榄岩和瑞士Arami石榴石橄榄岩的橄榄石中针状出溶体的研究为例,运用电子探针中的Map分析技术,很好地解决了图像与成分的对应性问题,使得测试结果真实、可信。
4) garnet lherzolite
石榴二辉橄榄岩
1.
Olivine fabric in garnet lherzolite from Rongcheng and Bixiling of Sulu-Dabieshan Ultrahigh-pressure(UHP)metamorphic belt,Eastern China.;
苏鲁-大别山超高压变质带迟家店和碧溪岭石榴二辉橄榄岩橄榄石组构
5) pyrope-olivinfels,pyrope-peridotite
镁铝榴石橄榄岩
6) garnet bearing peridotites
含石榴石橄榄岩捕虏体
补充资料：超高压
超高压
一般指高于一万大气压的压强。在超高压下，物质的物理化学性质发生显著变化。利用超高压和高温可使物质结构改变，或者合成自然界尚未发现过的物质，如固体氮和性质极硬的氮化硼等。
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