1) 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。
2) 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。
3) Ultra-high-pressune eclogite belt
超高压榴辉岩带
4) high-ultrahigh pressure transition eclogites
高压/超高压过渡榴辉岩
6) ultra-high-pressure eclogites and jadeite quartzite
超高压榴辉岩和硬玉石英岩
补充资料：榴辉岩
| 榴辉岩 eclogite 一种变质岩。由区域变质作用形成。主要由绿辉石和富镁的石榴子石组成。典型的榴辉岩不含斜长石，可含少量石英、蓝晶石、金红石、尖晶石等。具不等粒变晶结构及块状构造。有3种产出状态：①呈包裹体产于金伯利岩和层状超基性岩中。②呈夹层状、透镜体产于角闪岩相和麻粒岩相的岩石中。③呈夹层或透镜体产于蓝闪石-硬柱石片岩相岩石中。通常认为它是在极高压条件下形成的岩石，但温度变化范围较大。金伯利岩中的榴辉岩包体波认为是地幔物质的产物。 |
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