1) eclogite xenoliths
榴辉岩类捕虏体
1.
Abundant eclogite xenoliths are found in Mesozoic dioritic rocks from Xuzhou-Suzhou area,central China.
徐州-宿州地区中生代闪长质岩石中存在丰富的榴辉岩类捕虏体。
2) Eclogite facies garnet pyroxenolite xenoliths
榴辉岩相石榴辉石岩捕虏体
1.
Eclogite facies garnet pyroxenolite xenoliths in Hannuoba area show the typical layered cumulate structures and crystalloblastic textures of granulite facies.
汉诺坝榴辉岩相石榴辉石岩捕虏体的产状、层状堆晶构造和粒状变晶结构 ,以及具有幔源成因的矿物学、REE地球化学特征和温压条件表明 ,其深部过程是由幔源岩浆底侵于上地幔顶部 ,形成镁铁质堆晶岩 ,再经榴辉岩相变质而成 ,它与下地壳底部的麻粒岩相镁铁质堆晶岩 ,提供了岩浆底侵作用和壳 -幔过渡带存在的新证据。
3) the granulite-eclogite facies cumulate xenoliths
麻粒岩相-榴辉岩相堆晶岩捕虏体
4) pyroxenite xenolith
辉石岩捕虏体
1.
Abundant pyroxenite xenoliths were found from the Cenozoic Changle basalts,an area distributing near the Tanlu fault zone.
紧邻郯庐断裂带分布的山东昌乐新生代玄武岩含有丰富的辉石岩捕虏体。
2.
The major and trace element data of granulite and pyroxenite xenoliths, which are entrained in Hannuoba basalt Hebei Province, North China, suggest the highly chemical heterogeneity in the lower crust and crust-mantle transitional zone.
河北汉诺坝玄武岩中长英质麻粒岩、镁铁质麻粒岩和辉石岩捕虏体的主量元素和微量元素特征，反映了下地壳及壳幔过渡带组成具有高度化学不均一性。
5) garnet bearing peridotites
含石榴石橄榄岩捕虏体
6) clinopyroxenite xenolith
单斜辉石岩捕虏体
1.
Petrology and mineralogy of spinel-clinopyroxenite xenolith in Early Jurassic intrusive complex from Xu-Huai region, central China indicate that Mg-Fe spinel and Al-clinopyroxene assemblage could be present as the cumulate of the underplating magma in the lower crust or the most upper mantle, which were formed under 0.
对徐—淮地区早侏罗世侵入杂岩中尖晶石单斜辉石岩捕虏体的岩石学和矿物学研究表明 ,镁铁尖晶石和富铝单斜辉石矿物组合代表了更早期地幔岩浆在下部地壳或上地幔顶部的堆积体 ,其形成的温压条件为 0 。
补充资料：抄虏
1.抢劫虏掠。
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