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1)  garnet-bearing gneissic granite
含石榴子石片麻状花岗岩
1.
Hence the Laoshan garnet-bearing gneissic granite was derived from the partial melting of the crustal materials of the South China Block(SCB),which was suffered from the Triassic UHP metamorphism,or resulted from the recycling of the Triassic subducted continental crust of the SCB.
对华北板块东南缘蚌埠隆起区内凤阳县老山含石榴子石片麻状花岗岩进行了锆石SHRI MP U-Pb定年。
2)  garnet-bearing monzonitic granite
含石榴石二长花岗岩
1.
The garnet-bearing monzonitic granite intrusions are distributed in the Yanwan area along the northern side of the Shangxian-Danfeng faults in the western segment of Northern Qinling Mts.
北秦岭造山带西段商丹断裂带北侧岩湾一带分布的含石榴石二长花岗岩以含富铝的石榴石、白云母等矿物为特征,属含白云母过铝质花岗岩类(MPG);SiO2含量为73。
3)  garnet-bearing two-mica granite
含石榴子石二云母花岗岩
1.
SHRIMP zircon U-Pb age of garnet-bearing two-mica granite at Comai Township, Lhari County, Tibet, and its significance;
西藏嘉黎县措麦地区含石榴子石二云母花岗岩锆石SHRIMP U-Pb年龄及其意义
4)  crushed granite
花岗岩石子
5)  garnet migmatitic granite
石榴混合花岗质岩石
1.
Geochemical characteristics and origin of garnet migmatitic granites in Daqingshan area, Inner Mongolia;
内蒙古大青山地区石榴混合花岗质岩石地球化学特征及成因
6)  garnet-bearing granite
含榴花岗岩
1.
The garnet-bearing granites account for more than 85% in volume in the UHP units, with a mineral assemblage of Or+Ab+Q+Bi+Mc+Grt +Zr+Ep+Ae+Hb.
大别—苏鲁超高压地体中的面理化花岗岩因为常含石榴石而被简称为含榴花岗岩 ,其岩石类型主要为二长花岗岩、花岗岩和微斜长石花岗岩 ,岩石具有花岗结构和片麻状构造 。
补充资料:石榴子
1.石榴的子粒。 2.宝石名。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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