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1·The holocrystalline porphyritic olivine basalts and pyroclastic rocks are the components of Pleistocene to recent volcanic activities.

完整的斑状斑状橄榄石玄武岩和火山碎屑岩是最近火山活动的更新世的组成部分。

2·Lateritic crust of basalts is of zonal texture.

玄武岩红土壳具帝状结构。

3·The basalts of the Hutuo group might erupt in rift environment.

综合分析认为，滹沱群玄武岩可能形成于板内裂谷环境。

4·The chief type of Cenozoic basalts in Zhejiang is of olivine-tholeiites.

浙江新生代玄武岩主要岩石类型为橄榄拉斑玄武岩。

5·The erosion scope is coeval with the spatial distribution of the Emeishan basalts.

整个剥蚀区的范围同峨眉山玄武岩分布区基本一致。

6·In contrast, the less abundant HT and LT2 basalts may imply a weakening of the influence of the mantle plume activity.

相反，厚度较小的HT和LT2玄武岩则可能是意味着地幔柱活动影响的减弱。

7·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。

8·This series of Cenozoic volcanic rocks has obvious features of continental flood basalts, even its distribution is not widely.

这套火山岩虽然面积不是很大，但具有大陆溢流玄武岩的特点。

9·Helium isotope compositions of the mantle-derived xenoliths and megacrysts from the Cenozoic basalts in Hannuoba were measured.

对该地区新生代玄武岩中幔源包体和高压巨晶的氦同位素进行了初步研究。

10·The best reservoir rocks in the area are dissolution volcanic breccias, vesicular basalt and tight basalts with developed fractures.

溶蚀火山角砾岩，气孔玄武岩和裂缝发育的致密玄武岩是区内最好的储集岩类。

玄武岩

1·The holocrystalline porphyritic olivine basalts and pyroclastic rocks are the components of Pleistocene to recent volcanic activities.

完整的斑状斑状橄榄石玄武岩和火山碎屑岩是最近火山活动的更新世的组成部分。

2·Isotopic systematics of flood basalts indicate that their sources are involved in crust-mantle mixing in a recycled mantle, decompression melting of lithosphere.

溢流玄武岩的同位素体系特征表明它们的源区涉及再循环地幔的壳幔混合、岩石圈减压熔融、上—下地幔过渡带和似原始-略亏损的下地幔。

3·The best reservoir rocks in the area are dissolution volcanic breccias, vesicular basalt and tight basalts with developed fractures.

溶蚀火山角砾岩，气孔玄武岩和裂缝发育的致密玄武岩是区内最好的储集岩类。

4·Previous regional studies have suggested that the southern Philippines is a type locality for both adakites and Nb-enriched arc basalts.

先前的区域研究表明，南菲律宾是埃达克岩和富铌岛弧玄武岩的一个典型产地。

5·On the basis of batch-type melting model, the author explains the linear relationships between elements which are often recognized in oceanic basalts.

大洋玄武岩中，元素之间常常存在线性关系。本文应用批式熔融模型，解释了这一现象。