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玄武岩

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The calculated δ13C values of CO2 gas being in equilibrium with dawsonite ranged from -8.7‰ to-6.9‰ and was in coincidence with the δ13C values ranging from -9.76‰to -5.74‰ of CO2 gas in Gudian carbonate dioxide gas field.

由于含片钠铝石砂岩与CO2气的分布都受控于深大断裂和玄武岩,CO2气和形成片钠铝石的CO2绝大部分属于幔源岩浆型。

An inscription of a black basalt stone; gave first clue to decipherment of ''.

刻在黑色玄武岩上的一种碑铭;给出了''。

An inscription of a black basalt stone; gave first clue to decipherment of Egyptian hieroglyphics.

刻在黑色玄武岩上的一种碑铭;给出了解读埃及象形文字第一线索。

The homogeneous temperature, decrepitation temperature, major element compositions and volatile components of the inclusions were determined.

详细本文首次对冲绳海槽的浮岩和玄武岩中矿物的包裹体进行了系统的分析研究。

In this area, there are huge thick basalt and diabase wall clusters, which have been thought as the Mesoproterozoic basic magmatism.

此地区发育巨厚的玄武岩及辉绿岩墙群,过去认为系中元古代时期的基性岩浆活动。

Also on the analysis of geochemical data, it is sugested that the composition of eclogite is not simple butacombination of terrestriaI tholeiite and basic volcanic tuff and marl.

同时根据地球化学资料等分析,认为榴辉岩的成分不是单一的,一部分为大陆拉斑玄武岩、一为基性的火山凝灰岩和泥灰岩。

Geochemistrical research illustrated that the protogene of eclogite consistsed of various basalts in different tectonic setting.

地球化学研究表明,七角山岩组和浒湾岩组的榴辉岩原岩是形成于多种构造背景的玄武岩

Towering in close symmetry, these basalt columns near Fingal's Cave form the base of the Scottish island of Staffa.

高耸的密切对称性,这些玄武岩圆柱附近的芬戈尔洞形成的基底苏格兰岛屿的斯达法岛。

Photo Gallery: Extreme Earth Towering in close symmetry, these basalt columns near Fingal's Cave form the base of the Scottish island of Staffa.

高耸的密切的对称性,这些玄武岩园柱状物附近Fingal的洞穴形式的基础上苏格兰岛的Staffa 。

The uplifting belt is composed of metasandstone, marble, overlying thick stromatolite (Jinyanshan Group of Jixian System). Metamorphic rocks of 450Ma± occur in both south and north active margin. Post-collision bimodal volcanic rocks and A-type granite occur in the middle and the north side;(4) Apa-Mangya tectonic melange belt consists of ophiolite (including ultramafic rocks, gabbro, plagiogranite and basalt) and flysch and eclogite of late Ordovician.

隆起带为中元古界变砂岩、大理岩,上覆厚层叠层石灰岩,南北边缘有均为450Ma左右的变质岩,中部和北侧分布有碰撞后双峰式火山岩与碱性花岗岩;④阿帕—茫崖构造混杂岩带,由超镁铁质岩、辉长岩、斜长花岗岩、玄武岩等蛇绿岩残片与晚奥陶世复理石沉积和榴辉岩块组成。

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