1) Pengguan complex
彭灌杂岩体
1.
Study on the forming model of Pengguan complex of the Longmenshan orogenic belt
龙门山造山带彭灌杂岩体形成模式
2.
Pengguan complex formed in Meso-and Neoproterozoic was in tectonic emplacement between the Yinxiu fault and the Maowen fault.
形成于中——晚元古代的彭灌杂岩体构造侵位于映秀断裂和茂汶断裂之间。
2) Pengguan complex
彭灌杂岩
1.
The Pengguan complex,located in the Longmenshan thrust belt,western margin of the Yangtze block,SW China,was formed during the Neoproterozoic.
对位于扬子地块西缘龙门山逆冲推覆构造带中的彭灌杂岩进行了岩石地球化学研究,重点讨论了岩石成因、成岩物质来源及其构造意义。
2.
Pengguan complex as a nappe in the middle Longmen Mountains consists mainly of adamellite, tonalite, moyite and gabbro in the Middle-Late Proterozoic, with an isotopic age of 699-859 Ma by zircon, decollement fault (Yingxiu fault) is a brittle-ductile fault or a strike-slip reverse thrust predominated by brittle deformation.
位于龙门山中段的“彭灌杂岩”推覆体，主要由中晚元古代的二长花岗岩、英云间长岩、钾长花岗岩、辉长岩等组成，用颗粒锆石法测其年龄值为６９９—８５９Ｍａ。
4) rock mass grouting
岩体灌浆
1.
The detection methods of rock mass grouting and applicability evaluation;
岩体灌浆检测方法及其适用性评价
5) Peng-Guan area
彭灌地区
6) complex
[英]['kɔmpleks] [美][kəm'plɛks, 'kɑm,plɛks]
杂岩体
1.
Basic Characteristics of Jinxingtou Complex in Yiyuan County and the Relation with Gold Mineralization;
沂源县金星头杂岩体基本特征及与金矿化的关系
2.
Discussion on the Relation Between Basic Characteristics of Tiezhai Complex and Its Gold Mineralization in Linqu;
临朐铁寨杂岩体基本特征及其与金矿化关系的探讨
3.
1 complex at Tulaergen, Hami County, Xinjiang Uygur Autonomous Region.
从区域铜镍矿成矿地质背景、矿区地球物理、地球化学特征等方面入手,对图拉尔根①号杂岩体进行岩相、岩石化学特征及矿化蚀变分析,与黄山、香山成型矿床进行对比。
补充资料：雨花岩颂彭泽三岩
【诗文】：
孤峰中流分江南，马当大雷无一帆。
波涛抓空鸟不度，天花雨我读书岩。
【注释】：
【出处】：
孤峰中流分江南，马当大雷无一帆。
波涛抓空鸟不度，天花雨我读书岩。
【注释】：
【出处】：
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