1) shallow-source inclusion
浅源包体
2) mantle-derived xenoliths
幔源包体
1.
Laser-fluorination technique has been used to determine the O-isotopic ratios of mineral separates from mantle-derived xenoliths from the Yitong.
吉林伊通幔源包体的氧同位素组成徐义刚，Ｍ。
3) mantle xenolith
幔源包体
1.
Clinopyroxene-melt equilibrium temperature and pressure of Cenozoic basalts with special reference to the genesis of mantle xenoliths in some areas of eastern China;
中国东部几个地区新生代玄武岩中单斜辉石-熔体平衡温压——兼论幔源包体的成因
2.
The Quaternary basalts in Shandong Province contain mantle xenoliths of varied quantities and sizes.
山东省第四纪玄武岩中含有数量、大小不等的幔源包体。
3.
The mantle xenoliths collected from these three localities have been described in this paner.
中国东部含幔源包体的早第三纪玄武岩已发现的有吉林双辽、河北阳原和山西繁峙。
4) mantle xenoliths
幔源包体
1.
In eastern China there are more than one hundred reported localities of mantle xenoliths, on which a lot of studies have been carried out.
新生代火山岩中的幔源包体可以提供有关上地幔的直接信息。
2.
The upper mantle geotherm and rheology for Mingxi, Fujian Province, has been constructed through a detailed study of mantle xenoliths collected from this area.
通过对采自福建明溪的幔源包体样品的详细研究,建立了该区上地幔的地温线,探讨其流变学特征。
3.
Major, trace element composition and Sr-Nd-Pb isotopes of the Cenozoic basalts from Yangyuan (Hebei Province) and Datong (Shanxi Province), which are located to west of the Daxinanling-Taihanshan gravity lineament, as well as mineral chemistry, major and trace element composition and Sr-Nd isotopes of mantle xenoliths from Yangyuan are reported in this thesis.
本文报道了大兴安岭-太行山重力梯度带以西河北阳原和山西大同新生代玄武岩的元素和Sr-Nd-Pb同位素地球化学及阳原幔源包体的矿物化学、元素和Sr-Nd同位素地球化学，据此对华北克拉通西部上地幔的性质和过程进行了初步讨论。
5) mantle-derived xenolith
幔源包体
1.
This paper deals with deformation textures, petrofabrics and dislocation micros-tructures of olivine from the mantle-derived xenoliths in the Penghu Islands, Taiwan.
本文详细研究了台湾澎湖列岛上地幔幔源包体的变形结构、组构和橄榄石位错构造。
6) deepseated xenolith
深源包体
1.
There are abundant deepseated xenoliths in Nushan alkali basalts, Anhui province, such as lherzolites, pyroxenites, composite xenoliths and granulite xenoliths.
安徽女山碱性玄武岩中具丰富的各类深源包体：二辉橄榄岩包体、辉石岩包体、复合包体和麻粒岩包体等。
补充资料：教体浅深
【教体浅深】
教体浅深者，谓如来说教，必有其体。若演华严之教，则以海印三昧，及事事无碍为体。今通论一大藏教，从浅至深，略而明之，有十体也。（梵语三昧，华言正定。海印三昧者，谓大海澄渟，万像皆现，如印印物；如来智海，清净湛然，一切众生心念根欲，在如来三昧智中，犹海现像也。十体者，音声语言体、名句文身体、通取四法体、通摄所诠体、诸法显义体、摄境唯心体、会缘入实体、理事无碍体、事事无碍体、海印炳现体也。）
教体浅深者，谓如来说教，必有其体。若演华严之教，则以海印三昧，及事事无碍为体。今通论一大藏教，从浅至深，略而明之，有十体也。（梵语三昧，华言正定。海印三昧者，谓大海澄渟，万像皆现，如印印物；如来智海，清净湛然，一切众生心念根欲，在如来三昧智中，犹海现像也。十体者，音声语言体、名句文身体、通取四法体、通摄所诠体、诸法显义体、摄境唯心体、会缘入实体、理事无碍体、事事无碍体、海印炳现体也。）
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