1) plagioclase granite porphyry
斜长花岗斑岩
1.
It was reported that they were the same unit,and all the time denominated biotite plagioclase granite porphyry.
安徽省石屋岩体和岑山岩体在地质产状、形成时代及岩石学特征上十分相似 ,前人将其划为同一单元 ,并一直将其定名为黑云母斜长花岗斑岩。
2) plagiogranite
斜长花岗岩
1.
Geochronology,Geochemistry and Geological Implications of the Mengku Synorogenic Plagiogranite Pluton in Altay,Xinjiang;
新疆阿尔泰蒙库同造山斜长花岗岩年代学、地球化学及其地质意义
2.
U-Pb isotope zircon age of Baiyanhua plagiogranite in Seerteng area,Inner Mongolia;
内蒙古色尔腾地区白彦花斜长花岗岩锆石U-Pb年龄
3.
Dating and tectonic significance of plagiogranite from Guoganjianian Mountain,central Qiangtang, northern Tibet, China
藏北羌塘中部果干加年山斜长花岗岩定年及其构造意义
3) markfieldite
斜长花斑岩
4) granodiorite porphyry
花岗闪长斑岩
1.
SHRIMP U-Pb dating of zircons from granodiorite porphyry gravels in a conglomeratic lithic sandstone sample from this suite of rocks yields a weighted mean age of 314.
对其中含砾岩屑砂岩中花岗闪长斑岩砾石的锆石进行SHRIMPU-Pb定年,获得206Pb/238U加权平均年龄为314Ma±4。
2.
During the late stage of reverse napping,granodiorite porphyry emplaced along the nappe structure and hydrothermal ore-forming solution accumulated and formed gold deposits at favourable positions.
推覆构造形成于 J2-J3，逆冲推覆后期，花岗闪长斑岩沿逆冲推覆构造就位，其所携带的成矿热液在有利部位富集成金矿。
5) monzogranite-porphyry dike
二长花岗斑岩脉
1.
Zircon SHRIMP U-Pb dating of monzogranite-porphyry dikes in Shengongcun, northern Zhejiang, and its geological implications;
浙北富阳神功村二长花岗斑岩脉SHRIMP锆石U-Pb年龄及其地质意义
6) rapakivi granites
奥长环斑花岗岩
1.
This paper introduces the connotation of rapakivi texture and geological and geochemical characteristics of rapakivi granites.
本文介绍了环斑结构的含义及奥长环斑花岗岩的地质与地球化学特征。
补充资料：高地斜长岩
分子式：
CAS号：
性质：主要分布在月球高地的富含镁的结晶岩和钾、稀土、磷的岩类。斜长岩由95％的斜长石及少量低钙辉石组成。斜长岩是岩浆分异或残余熔浆结晶形成的富含挥发分元素的岩石,87Sr/86Sr比值极低。
CAS号：
性质：主要分布在月球高地的富含镁的结晶岩和钾、稀土、磷的岩类。斜长岩由95％的斜长石及少量低钙辉石组成。斜长岩是岩浆分异或残余熔浆结晶形成的富含挥发分元素的岩石,87Sr/86Sr比值极低。
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