1) High-Ti eclogite
高-Ti榴辉岩原岩
2) UHP eclogite
超高压榴辉岩
1.
The formation of nanometer twins of rutile and its textural characteristics in UHP eclogite.;
超高压榴辉岩中金红石的纳米级微构造特征及成因机制探讨
2.
Deformation features of gneiss and UHP eclogite from ductile shear zone and its relation with seismic velocity anisotropy: Evidences from core samples at depth of 680 ~ 1200m of CCSD;
韧性剪切带中片麻岩和超高压榴辉岩变形特征及其与地震波速各向异性的关系:来自中国大陆科学钻探(CCSD)680～1200米岩心的证据
3.
There still have been some disputable opinions on the UHP eclogites in western Dabieshan,especially regarding the stability of glaucophane-and kyanite-bearing assemblages in eclogites,their peak PT conditions and mineral assemblages,and the mineral evolution and fluid activity during early HP retrograde stage.
目前对于大别山西段超高压榴辉岩仍存在一些不清楚的问题和模糊的认识,如蓝闪石和蓝晶石组合的稳定范围,峰期温压条件和矿物组合,以及早期退变质过程的矿物演化和流体作用。
3) ultrahigh pressure eclogite
超高压榴辉岩
1.
The understanding of deformation mechanism from ultrahigh pressure eclogite is crucial for the construction of geodynamic models of orogenic belt.
详细介绍了绿辉石ＬＰＯ测定方法和步骤，报道了潜山县双河地区超高压榴辉岩中绿辉石组构初步研究成果及流变学意义。
4) Ultra-high-pressune eclogite belt
超高压榴辉岩带
5) high Fe-Ti eclogite
高铁钛榴辉岩
1.
The high Fe-Ti eclogites appear at the depth intervals from 318-380m (A),420-470m (B) and 530-600m (C) respectivelys in the Chinese Continental Scientific Drilling (CCSD) Project main hole.
中国大陆科学钻探(CCSD)主孔中318～380m(A)、420～470m(B)和530～600m(C)深度分布三段高铁钛榴辉岩,它们具有高全铁(FeOT)(平均15。
6) eclogite
[英]['eklədʒait] [美]['ɛklə,dʒaɪt]
榴辉岩
1.
SHRIMP U-Pb ages and inclusions of zircons from the Sumdo eclogite in the Lhasa block, Tibet,;
青藏高原拉萨地块松多榴辉岩的锆石SHRIMPU-Pb年龄及锆石中的包裹体
2.
Petrography and metamorphic evolution of the Sumdo eclogite, Qinghai-Tibetan Plateau.;
青藏高原拉萨地块松多榴辉岩的岩相学特征和变质演化过程
3.
Oceanic subduction-type eclogite in the Lhasa block, Tibet, China:Remains of the Paleo-Tethys ocean basin?;
青藏高原拉萨地块中的大洋俯冲型榴辉岩:古特提斯洋盆的残留?
补充资料：妙高岩
妙高岩位于白龙洞的右上方。在洞顶的悬崖上刻有“日照岩”三个字。当金山还耸立在江中的时候，每当旭日冉冉东升，妙高岩向南的一带石壁上，金碧辉煌，水天皆赤，顿成奇观。故这里是观日出的最佳之处。
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