1) The Xiaoqinling metamorphic core complex
小秦岭变质核杂岩
1.
The Xiaoqinling metamorphic core complex experienced two stages of extension with different mechanism.
作为中国金矿主产地之一 ,小秦岭变质核杂岩经历两期不同性质的伸展。
2) Qinling core complex
秦岭核部杂岩
1.
9 ), It is in-terpreted as the age of the isobaric cooling event of statically crystallized carbonate minerals in rnarbles, reflect1ng approximately the age of uplifted Qinling core complex aftar thickening due to collision.
本文报道了豫西东秦岭核部杂岩中大理岩919±53Ma的Ph－Pb等时线年龄测定结果，结合本地区变质作用及其年龄研究结果，指出大理岩919±53Ma的Pb-Pb等时线年龄是碳酸盐岩区域变质作用形成大理岩后近于等压冷却的年龄,为秦岭地区加厚的地壳均衡隆升，到达地壳一定深度后近于等压的冷却提供了同位亲年龄证据。
3) Qinling complex
秦岭杂岩
1.
Characteristics of metamorphic intrusion in Qinling complex;
秦岭杂岩中变质侵入体特征
2.
Brief Review of the Study of Qinling Complex,Qinling Orogenic Belt;
秦岭造山带秦岭杂岩研究中有关问题讨论
3.
Discovery and significance of high-pressure impure marbles in Qinling complex east Qinling;
秦岭杂岩残存高压不纯大理岩的确定及其意义
4) Metamorphic core complex
变质核杂岩
1.
Rotation of crustal blocks as an explanation of Oligo-Miocene extension in Southeastern Tibet—evidenced by the Diancangshan and nearby metamorphic core complexes;
用陆块旋转解释藏东南渐新世—中新世伸展作用——来自点苍山及邻区变质核杂岩的证据
2.
A review on the characteristics and the genesis of metamorphic core complexes;
变质核杂岩特征及小秦岭地区变质杂岩成因讨论
3.
Some characteristics of metamorphic core complexes;
关于变质核杂岩构造特征的几个问题
5) metamorphic core
变质杂岩核
1.
There are typical complex structures of the metamorphic core within the small Qinling region at the south fringe of the North China.
华北古地台南缘的小秦岭地区呈现为一典型的变质杂岩核构造。
6) metamorphic core complexes
变质核杂岩
1.
Definition and significance of the Lhagoi Kangri metamorphic core complexes in Sa gya,southern Tibet;
藏南萨迦拉轨岗日变质核杂岩的厘定及其成因
2.
There are many lamprophyric and othr magmatic dike groups in the main detachment fault of metamorphic core complexes in Hebei province.
研究河北省变质核杂岩构造时发现:在主拆离滑脱带内,可见成群成组产出的煌斑岩及其他浅成脉岩。
3.
Two uplifts in the Taihang Mountains area,Fuping and Zanhuang,are the typical metamorphic core complexes resulted from extensional tectonics during the Meso Cenozoic era.
阜平、赞皇隆起是太行山地区中新生代伸展体制控制的变质核杂岩。
补充资料：登秦岭半岩遇雨
【诗文】：
屏翳忽腾气，浮阳惨无晖。千峰挂飞雨，百尺摇翠微。
震电闪云径，奔流翻石矶。倚岩假松盖，临水羡荷衣。
不得采苓去，空思乘月归。且怜东皋上，水色侵荆扉。
【注释】：
【出处】：
全唐诗：卷236_54
屏翳忽腾气，浮阳惨无晖。千峰挂飞雨，百尺摇翠微。
震电闪云径，奔流翻石矶。倚岩假松盖，临水羡荷衣。
不得采苓去，空思乘月归。且怜东皋上，水色侵荆扉。
【注释】：
【出处】：
全唐诗：卷236_54
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