pyrope

基本解釋

Red pyrope is one of the most important gem resources in Yunnan.
紅色的鎂鋁榴石是雲南最重要的寶石資源之一。
The variety of garnet includes almandine, pyrope, magnesium-iron garnet, manganese-aluminum garnet, andradite and calcium-chromium garnet.
石榴石的種類包括（鉄鋁榴石、鎂鋁榴石、鎂鉄榴石、錳鋁榴石、鈣鉄榴石、鈣鉻榴石）。
The garnets of M-type belong to pyrope mainly formed near the boundary between lithosphere and aesthenosphere under the megatemperature and ultrahigh pressure of Jinning or earlier orogeny.
型榴煇巖的石榴石屬鎂鋁榴石，形成於晉甯期高溫超高壓條件下的巖石圈與軟流圈交界附近。
The research shows that Cr3+ ion isresponsible for the red color of pyrope. According to the content of Cr3+ ions in the pyrope, the pyropescan be divided into three types: chromium-bearing pyrope, microchrominn-bearing prrope and pgrope.
研究得知，Cr3+離子是紅色的主要色素離子，根據其含量的不同，可分爲三種類型：含鉻鎂鋁榴石、微鉻鎂鋁榴石和鎂鋁榴石。
The EOS data of pyrope in high pressure region measured in DAC technique by using Ar as pressure transmitting medium has been found to be different from that obtained by using methyl and ethyl alcohol mixture as pressure transmitting medium.
採用氬氣作傳壓介質測得的狀態(tài)方程數(shù)據,在高壓區(qū),與酒精溶液作傳壓介質的情況極爲不同。