1) Inclusion thermometry
包体测温
2) inclusion
包体
1.
From inclusion and Ro data, it is clear that Pingbei strata had undergone a higher temperature gradient in geological history, which is favorable for source rock evolution.
从包体测温和镜质体反演资料推测平北工区经历了高于今地温梯度的热历史，这对平湖组烃源岩或深部烃源岩演化有利。
2.
Fracture model of samples with inclusion of high elastic modulus and different strength are simulated by using Northeastern University Centre of Rock Induced Seismicity Research(CRISR) RFPA 2D code.
应用东北大学岩石破裂与失稳研究中心开发的RFPA2D系统 ,对含高弹模不同强度的包体试样的破裂模式进行了数值试验 。
3.
Fracture model of samples with inclusion of low elastic modulus and different strength under the iso-speed displacement load are simulated by using our RFPA 2D code.
应用自行开发的岩石破裂与失稳RFPA2D系统 ,对含低弹模不同强度的包体试样的破裂模式进行了数值试验 。
3) xenolith
包体
1.
The deep lithological section in southern Hunan province──evidence from some xenoliths in alkaline basalt;
湘南地区深部岩石剖面的建立——来自深源岩石包体的证据
2.
Geochronology and geodynamic implications of the felsic granulite xenoliths from the Hannuoba Basalt;
汉诺坝长英质麻粒岩包体同位素年代学及其地球动力学意义
3.
There are anhydrous and hydrous granulite xenoliths from crust in basalt dated late Yanshan Period in Hunan Province, China.
湖南道县玄武岩中的麻粒岩包体属辉石麻粒岩类,其稳定矿物组合为斜长石-单斜辉石-斜方辉石-尖晶石-角闪石。
4) xenoliths
包体
1.
Geological and Geochemical Characteristics of Anatectic Xenoliths and the Model of lithosphere in Xingyang, Henan;
信阳深源包体的地质地球化学特征及其岩石圈模型
2.
There are a lot of spinel-lherzolite xenoliths in the Taiyangshan Mesozoic basalt in Ningyuan, Hunan province.
湖南宁远太阳山中生代玄武质火山岩内,产较丰富的尖晶石二辉橄榄岩包体。
3.
Deep-seated source xenoliths of peridotite,gabbro and intermediate acidic hornblende granulite occur in Early Cretaceous basalts,South Hunan Province.
湘南早白垩世（１３２～１３５）Ｍａ基性火山岩中含有橄榄岩类、辉长岩类、角闪麻粒岩相酸性岩包体，这三类包体的岩石学特征及地球物理参数（ｖｐ，ρ），分别与岩石圈地球物理模型中的上地幔，下地壳及中地壳相吻合。
5) enclave
包体
1.
Enclaves in Mid-acid Intrusive Rocks: Types, Discriminations, Studied Examples and Its Geological Significance;
中酸性侵入岩包体的类型、鉴别、研究实例及其地质意义
2.
The dark colored,microgranular and igneous-texture enclaves provide reliable evidence that indicates the existence of magma mingling.
暗色、细粒且具火成结构的岩石包体是指示岩浆混合作用存在的可靠证据。
3.
Dioritic enclaves of the Lisong Granite in Guangxi Province of China are know to have been originated from different magma sources on the basis of their features like occurrence, texture and petrochemistry.
根据产状、岩石结构与岩石化学等特征,确定里松花岗岩中闪长质包体为异源岩浆岩成因。
6) melt inclusion
熔融包体
参考词条
补充资料：包析体
peritectoid：合金于冷却时发生包析相变所形成的产物。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。