对山东高压-超高压变质带的几点看法——程裕淇院士野外考察记  

SOME OPINIONS ABOUT HIGHULTRAHIGH PRESSURE METAMORPHIC BELT IN SHANDONG

作　　者：徐惠芬[1] 

机构地区：[1]中国地质科学院地质研究所

出　　处：《山东地质》1998年第4期1-3,共3页Geology of Shandong

摘　　要：通过对山东高压超高压变质带的考察，初步认为：榴辉岩的最后隆升时代为燕山期；含硬玉石英岩＋榴辉岩＋（透辉石）大理岩组合说明表壳岩经历了高压超高压变质作用；该带晋宁期长英质片麻岩花岗岩广泛出露；在其北部麻粒岩和榴辉岩密切伴生。After visiting the highultrahigh pressure metamorphic belt in Shandong,some opinions about it stated by professor Cheng Yuqi,an academician of Chinese academy of sciences:the last lifting period of eclogite belongs to Yanshan stage;the combination of jadeitebearing quartzite, eclogite and (diopside)marble shows that the supracrustal rock experienced highultrahigh pressure metamorphism; felsic gneissgranites of Jinning stage widely overcropped in this area;gneiss and eclogite occur accompaniedly in its north part.

关 键 词：高压-超高压 变质带 榴辉岩 麻岩 花岗岩 变质岩 

分 类 号：P588.3[天文地球—岩石学]