1) Linglong granitoid batholith
玲珑花岗岩基
2) Linglong granite
玲珑花岗岩
1.
This suggests that the Linglong granite is crustal origin, and that the i.
胶东招掖玲珑花岗岩锆石ＳＨＲＩＭＰＵ－Ｐｂ年龄结果表明，玲珑花岗岩形成于中生代燕山期（岩浆锆石年龄为１５０～１６０Ｍａ之间），岩体中产有大量的中生代印支期继承锆石（２００～２５０Ｍａ）及少数前寒武纪继承锆石。
4) Linglong
玲珑
1.
Inference of the three_dimensional geometry of the Linglong granitic complex at depth from 2_D gravity forward modeling, constrained by geological data, Shandong Province, East China, is presented.
根据胶东地区西北部的重力资料 ,并在地质资料的约束下 ,采用人 -机联作的二维模拟方法 ,对玲珑花岗质杂岩体三维形态进行了细致的推断 。
2.
Linglong gneissic granite as the initial material, a series of partially melting experiments were carried out under both pure water and H2O-CO2 mixture (x(H2O)=0.
以玲珑片麻状花岗岩为初始物，采用纯水和Ｈ２Ｏ－ＣＯ２混合物（ｘ（Ｈ２Ｏ）＝０。
5) granitic batholith
花岗岩基
1.
SHRIMP U-Pb zircon dating of the Dushan granitic batholith and related granite-porphyry dyke, eastern Hebei Province,;
冀东都山花岗岩基及相关花岗斑岩脉SHRIMP锆石U-Pb法定年及其意义
2.
The Dangchuan granitic batholith,which is located in the conjunction area of the Qilian and the North Qinling orogenic belts,is composed of 9 granitic intrusive bodies,whose rocks are rich in K_2O generally.
党川花岗岩基产于祁连与北秦岭造山带结合部位,由9个岩体组成,岩石普遍富K2O。
3.
Located in the area of the Qilian and west Qinling orogenic belts,the Dangchuan granitic batholith is composed of 9 granitic intrusives.
党川花岗岩基产于祁连与北秦岭造山带结合部位,由9个岩体组成,岩石普遍低Ga、Rb、Zr、高Th、Ta、Hf,富集重稀土元素。
6) granitic bedrock
花岗质基岩
1.
On the base of study of petrochemistry trace element geochemistry and geochronology,thegranitic bedrock and it's inclusion in Nanbao depression of East Hebei is shown to be formed in thedeep part of crust and had been assimilated-mingled strongly in uper crust.
通过对高参１井岩石化学、地球化学（含微量元素地球化学）及年代学的研究，确定本区花岗质基岩及其包体形成于地壳深部，并被上部地壳同化混杂。
补充资料：登玲珑山
【诗文】：
何年僵立两苍龙，瘦脊盘盘尚倚空。
翠浪舞翻红罢亚，白云穿破碧玲珑。
三休亭上工延月，九折岩前巧贮风。
脚力尽时山更好，莫将有限趁无穷。
【注释】：
【出处】：
苏轼诗集 卷五
何年僵立两苍龙，瘦脊盘盘尚倚空。
翠浪舞翻红罢亚，白云穿破碧玲珑。
三休亭上工延月，九折岩前巧贮风。
脚力尽时山更好，莫将有限趁无穷。
【注释】：
【出处】：
苏轼诗集 卷五
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