南京大学学报(自然科学版) ›› 2013, Vol. 49 ›› Issue (3): 356393.
夏斌1.2,刘维亮1.2**,周国庆3,韦振权2.4,王冉2.5,李建峰2,钟云1,胡西冲1
Xiu Bin1’2,Liu Wei一Lung 1’2 ,Zhou Guo一Qing3,Wei Zhen一Quan2,4,Wang Ran2.5
Li Jian Feng 2,Zhong Yun1,Hu Xi-Chong1
摘要: 西藏蓬湖西发现了有别于一般榴辉岩和石榴石辉石岩的超高压镁质榴辉岩,具有平衡变晶结
构,广泛发育复杂多期的出溶结构.根据矿物出溶关系可分出三个世代的单斜辉石(Cpx)和三个世代的
石榴石(Grt)和对应地三个单斜辉石(Cpx)一石榴石(Grt)对,此外还有出溶的斜方辉石、铝铬铁矿和钠长
石.对具代表性的单斜辉石一石榴石和单斜辉石一斜方辉石矿物对,得到三个阶段温度压力:阶段III一1的
平衡条件为4GPa和1113?C一1129 ?C;阶段III- 2的平衡条件为3GPa和863?C一1033?C;阶段III一3
平衡条件为2 GPa和502?C -667?C.蓬湖西镁质榴辉岩P-T路径经历了三个阶段:阶段I,蓬湖西榴
辉岩形成,压力范围可能为0. 5 -1. 5GPa;阶段II,特提斯洋关闭,洋壳向深部俯冲,致使镁质榴辉岩从
尖晶石二辉橄榄岩稳定域穿过石榴石二辉橄榄岩稳定域并最终到达1400?C和5GPa的柯石英稳定域,
形成了在超高压条件下结构均一的、稳定的“单斜辉石+石榴石+斜方辉石”固溶体;阶段III,洋壳折返
过程中温度和压力降低使得原来稳定的“单斜辉石+石榴石+斜方辉石”固溶体发生出溶作用,形成多
期次、多种类型的出溶物.阶段III再分为三个次阶段,其温压变化范围大,为2 - 4 GPa, 502?C
1129?C.镁质榴辉岩中矿物出溶肯定与压力一温度降低有关.
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