| 1. | Xenoliths are found at numerous horizons, and locally there is evidence of scour and other erosional features .
捕虏体可见于许多层位，并局部可见到冲刷和其他侵蚀特征。
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| 2. | Significances of deep - seated xenolith in cretaceous basalt of inner mongolia
内蒙古四子王旗早白垩世深源捕虏体的发现及意义
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| 3. | Lattice preffered orientation and seismic anisotropy of ultramafic xenoliths in damaping , hebei province
河北大麻坪超基性岩包体的岩石组构和地震波速各向异性
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| 4. | A suit of highly potassic basalt bearing deep - source xenoliths has been discovered recently in the siziwangqi area , inner mongolia
内蒙古四子王旗地区发现含有深源捕虏体的富钾玄武岩。
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| 5. | Significances of deep - seated xenolith in cretaceous basalt of inner mongolia significances of deep - seated xenolith in cretaceous basalt of inner mongolia
内蒙古四子王旗早白垩世深源捕虏体的发现及意义
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| 6. | The xenoliths in the yangyuan , including iherzolite and harzburgite , represent the direct samples from the upper mantle beneath western north china craton
阳原幔源包体包括二辉橄榄岩和方辉橄榄岩，是华北西部上地幔的直接样品。
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| 7. | The lpo of main minerals of ultramafic xenoliths including spinel lherzolite , spinel harzburgite and plagioclasebearing websterite which collected from damaping , hebei province is analyzed and the seismic velocities of the rocks in
结果表明： 1大麻坪包体中橄榄石与斜方辉石的lpo方位关系与通常所见的100
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| 8. | A great number of lherzolite xenoliths occurs within the volcanic clastics characterized by terrigenous central type eruption at tianyang , jiudouyang and yingfenglin of qingtongyang , of southern leizhou peninsula
摘要雷州半岛南部田洋、九斗洋及青桐洋的英峰岭等陆相中心式喷发的火山碎屑岩中，分布有大量的二辉橄榄岩包体。
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| 9. | Siziwangqi of inner mongolia is located on the north margin of north china craton , the junction of north china craton and siberia . granulite xenoliths are found there in cretaceous basalt . these xenoliths are mainly plagioclase - pyroxenite
内蒙古四子王旗地区地处华北板块北缘，与西伯利亚板块的接合部，其早白垩世橄榄玄武岩中发现大量下地壳麻粒岩捕虏体，并可见辉石长石捕虏晶。
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| 10. | The early tertiary alkali basalts from yangyuan which contain abundant mantle xenoliths exhibit very homogeneous sr - nd isotopes with snd = 5 . 5 . their pb isotopes are similar to those of the depleted mantle ( dm ) and their trace element characteristics resemble those of oceanic island basalts ( oib )
含幔源包体的阳原早第三纪碱性玄武岩具有均一的sr - nd同位素组成( nd 5 . 5 ) ，其pb同位素组成与亏损地幔( dm )相似。
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