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陆壳

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Which results in the formation of a piedmont depression and accretion and thickening of continental crust.

导致山前坳陷带的形成和陆壳的加积、增厚。

The lithogeochemical study suggests that the Pana Formation volcanic rocks were formed about 40 Ma by anatexis of the thickened continental crust in the postcollision process between Indo plate and Eurasia plate.

研究表明,扎雪地区帕那组火山岩是40 Ma左右陆壳加厚并部分熔融形成的,是印度板块和欧亚板块后碰撞作用的产物。

This paper studies the granite growth, development and emplacement as well as their relations to the tectonic dynamic background and to reaction of ocean crust, continental crust and mantle. Thus, not only the contents of pluton study are enriched, but also new evidence for the tectonic evolution, plate kinematics and dynamics are obtained, indicating that the study of formation process and deformation reworking of plutons can provide more information on plate tectonic and continent dynamics, so they should be studied more.

本文研究了花岗岩体的成因、生长演化、形成定位及与构造动力学背景的关系,并注意与陆壳、洋壳、地幔三者之间相互作用的关系,这样,一方面丰富了花岗岩研究内容,提高了花岗岩研究程度;另一方面也对探索东秦岭地区大地构造演化及动力学等问题提供了新的证据和认识,表明在板块构造、大陆动力学研究方面,花岗岩体形成过程等方面的研究也能提供难得的信息,今后应注意加强研究。

Then followed by an apparent isobaric colling process with the appearance of an anti-clockwise PTt path, which implicates extension and thinning of the continental crust with the formation of thick sedimenting sequences in early stage, and the closure of rifted basin accompanied by slightly tectonic thicken under a compression regime in late stage.

采用石榴石微区温压计对儿个典型富铝片麻岩样品的估算结果显示,荆山群富铝岩系变质峰期的温度为720~770℃,压力为0.6~0.68GPa,峰期后存在较明显的近等压冷却过程,PTt轨迹为逆时针样式,反映陆壳先拉张减薄并接受沉积,后又挤压增厚的壳内裂陷带发育及闭合过程。

West Sarawak, which located in the Northwest of Kalimantan island, geotectonically underwent geosynclinal, platform periods and now in diwa process. The geological and structural features of Lupar River regionhe west part of West Sarawak?

位于加里曼丹岛西北部的西砂捞越地区,大地构造经历了地槽、地台和地洼三个演化阶段,西砂捞越西部卢帕河地区的地质构造特征代表了自晚白垩世到渐新世期间北东洋壳对南西陆壳的汇聚挤压作用。

In accordance with the characteristics of the occurence and tectonic emplacement of the ophiolitic belt.

目前认为蛇绿混杂岩带是洋盆闭合时洋壳残片构造侵位到陆壳之中的产物,为无序层序,相当于造山带非史密斯地层学划分类型的构造混杂体类,即由构造包体和基质两大部分组成。

The geochemical studies of the basalts indicate crustal contamination increases from the inland to the coast along the volcanic belt, and therefore show different degrees of crustmantle interactions.

研究表明,该火山岩带自西向东表现出不同程度的壳幔相互作用,玄武岩在成岩过程中有少量陆壳组分加入。

One is the continental crust and the other is the oceanic crust .

一种是陆壳,另一种是洋壳。

And changes to continental crust from mixed crust.

由混合壳转化为陆壳

And changes to continental crust from mixed crust.

即沉积结皮和结构结皮。8。由混合壳转化为陆壳

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