1) Lincang granitoid batholith
临沧花岗岩基
1.
Cenozoic cooling history of Lincang granitoid batholith, western Yunnan:Evidence from fission track data;
滇西临沧花岗岩基新生代剥蚀冷却的裂变径迹证据
2) 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。
3) 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。
4) Granite basement
花岗岩基底
5) granite batholith
花岗岩岩基<地>
6) Linglong granitoid batholith
玲珑花岗岩基
补充资料：沧沧凉凉
1.沧凉。
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