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岩基

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As one of major mineral phases in the intermediate-mafic intrusions in Southern Taihang Mountains , amphibole can be used to constrain its petrogenesis.

角闪石作为南太行山地区中基性侵入岩中主要组成矿物,其详细的成因矿物学研究对了解该套岩石的形成机理具有重要意义。

The mineral assemblage of mafic-intermediate lavas mainly contains pyroxene and plagioclase, and rarely with amphibole and bitotite.

中基性熔岩的主要造岩矿物是斜长石和辉石,几乎没有角闪石和黑云母。

The origin of the No. 7 nugget found in south suburbs of Yiyang city of Hunan mainly comes from plaeovolcanic rock and the gold veins and the basic volcanic clastic rock in Nenjiaxi Group slate around the plaeovolcanic rock. Its origin belongs to near source or autochthon sedimentary regeneration.

湖南益阳南郊 7号"狗头金"的金源主要来自古火山岩及其边部冷家溪群板岩中的含金矿脉与基性火山碎屑岩系,属近源甚至近于就地的沉积再生成因。

Leaves laterally flattened, basally equitant, sword-shaped; bracteole cupular; pedicel glabrous; anthers ovate, with 2 separate locules

叶侧面使变平,基部套折,剑形;小苞片杯状;花梗无毛花药卵形,具分开子房室 1 Tofieldia 岩菖蒲属

However, it is unsubstantial for the investigation on chorology and geochemisty, and dissimilar for the research on petrogenesis and tectonic setting. Therefore, based on the isotopic chorology, petrochemistry, geochemisty and Sr, Nd, Pb isotope, the Ph.

山东地区中生代基性脉岩特别发育,这些幔源基性岩脉充填张性裂隙,是大陆地壳拉张的标志;另外,山东地区也存在大量拉张背景下的燕山期火山岩和碱性岩。

Based on statistical results and the volcanic lithology and facies map, high cracks surface pore concentrates at diatreme subfacies and cryptoexploisve sub-facies of volcanic conduit facies, inner subfacies of extrusive facies, pyroclastic flow subfacies and base surge subfacies of explosive facies, lower subfacies of effusive facies which are close to the volcanic edifices center. Holes surface pore focus on upper and middle subfacies of effusive facies which locates in the edifice slope.

将物性结果结合平面岩性岩相图,确定出裂缝面孔率高的区域主要集中在火山机构中心附近的火山通道相火山颈亚相和隐爆角砾岩亚相、侵出相内带亚相、爆发相热碎屑流和热基浪亚相、喷溢相下部亚相;气孔面孔率高的区域集中在距离火山口较近的斜坡处,亚相主要为喷溢相上部、中部亚相。

This age represents the timing of the high pressure metamorphism that led to the formation of the Sumdo eclogite.

以松多榴辉岩为代表的洋壳俯冲事件同时表明带状基墨里大陆的形成有可能是一系列微陆块碰撞拼贴而成。

It is mainly ralated with two factors:(1) the degree of soil eluviation and rock erode;(2) the groundwater residence time.

2洞穴滴水的微量元素Ba~(2+除外含量及比值都呈现出一定的季节性变化,主要与两方面因素有关:1土壤淋漓和基岩溶蚀程度;2水岩作用时间长短。

Field geology characteristics show that they are composed of melange bases (mainly abyssal flysch and carbonate rocks) and melange blocks from various tectonic environments, often with fault contact among each lithological units, belonging to typical ophiolitic melange zone.

野外地质特征表明它们由混杂基质(主要为深海复理石和碳酸盐岩)和来自不同构造环境的混杂岩块组成,各岩石单元之间多以断层接触,属于典型的蛇绿混杂带。

Methylation analysis showed it contained 1,2- fucose linkage,1,4-, 1,4,6- and terminal glucose linkage.

甲基化分析结果表明,岩藻糖以1,2-方式连接,葡萄糖主要以1,4-、1,4,6-和端基的形式连接。

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