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protective belt相关的网络例句

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The main tectonic features of the four stages mentioned above can be summarized as follows, gneissic basement and greenstone belt in the Archean, formation and rifting of ancient continental crust in the Transition, creation and disposal of the first supercontinent Columbia in the Paleoproterozoic-Mesoproterozoic, and the assembly and disassembly of the supercontinent Rodinea under plate tectonic framework in Neoproterozoic.

这四大阶段的主要构造面貌分别是:片麻岩基底和绿岩带盆地,古陆壳的形成与裂解,第一个超级大陆即哥伦比亚超大陆的形成与离散,板块构造体制下罗迪尼亚超大陆的汇聚与离散,反映了大陆岩石圈的形成和由低级向高级的演化,因而每一阶段都有不同于前一阶段的沉积建造、火成岩类型及组合、变质作用、构造样式、构造线方向、变形方式和成矿作用。

In this paper, we report our structure observation and U-Pb zircon ages of the two types of Triassic granites, and use these data to place chronological constraints on the tectonic evolution of the western Kunlun orogenic belt. The gneissic garnet-bearing granite was crystallized at 241 Ma, whereas the horblende-bearing granite emplaced at 228 Ma.

对西昆仑西段海西晚期两类构造特征完全不同的花岗岩露头尺度的观察、锆石U-Pb定年结果表明,一类含石榴子石片麻状花岗岩形成时代为240.5±1.8 Ma,表现出同造山过程中的花岗岩变形特征;另一类块状含角闪石花岗岩的年龄为228.2±1.5 Ma。

According to the research of the paper, the "migmatite" of the Sizishan Formation, Xingdong Group distributed in northern Xiao Hinggan Mountains should be a suit of gneissic quartz monzonitegranite intrusions. Their whole rockmineral Rb-Sr isochronic dating is (482±19) Ma, indicating that an Caledonian magmatic events existed in the giant granitic belt of the Xiao Hinggan Mountains.

研究表明,分布于小兴安岭北部金林林场的兴东群四子山组&混合岩&为一套片麻状石英二长岩-花岗岩侵入体,岩石全岩-矿物Rb-Sr等时线年龄为(482±19) Ma,这表明小兴安岭巨型花岗岩带中存在早古生代岩浆事件。

Gnomonic charts are published covering the Atlantic, Pacific and IndianOceans, except for an equatorial belt in each ocean.

出版大圆海图覆盖大西洋,太平洋和印度洋(各大洋近赤道带水域除外)。

Gnomonic charts are published covering the Atlantic, Pacific and Indian Oceans, except for an equatorial belt in each ocean.

出版大圆海图覆盖大西洋,太平洋和印度洋(各大洋近赤道带水域除外)。

L Navigational Charts Gnomonic charts are published covering the Atlantic, Pacific and Indian Oceans, except for an equatorial belt in each ocean.

出版大圆海图覆盖大西洋,太平洋和印度洋(各大洋近赤道带水域除外)。

In southern Tianshan fold belt,there are large voluminous granitoid rocks.

在南天山褶皱带,分布有大量的花岗岩类岩石。

Because new mantle inputs have not been identified in terms of zircon Hf isotopes, mantle-derived magmas might not have been involved in formation of this S-type granitoid belt.

因为缺少显著幔源特征的高εHf值锆石,本文认为地幔物质基本没有参与该S型花岗岩带的形成。

This is an A_1 type granitoid belt, slightly predominated by mantle components. Their source regions are probably mainly the lithospheric mantle and lower crust, which had been metasomatized and enriched so that they could bear OIB characters in trace elements.

这是一个以地幔物质略占优势的A1亚型花岗质杂岩带,其源区物质可能主要是经过交代和富集的具有OIB型微量元素特征的岩石圈地幔和下地壳。

The eclogites at western segment of Altyn Tagh tectonic belt occur as lens or boundins within quratz-feldspathic gniesses characterized by amphibolite-facies parageneses. It mainly experienced the prograde amphibolite-facies stage (P=6.06-8.70kb, t=615-690℃),peak eclogite-facies stage (P>15kb,T=700-850℃), granulitic facies stage (P=11-14kb,T=750℃) and ampbiolite-facies stage (P=6.3-9.5kb,T=619-738℃) during decompression.

阿尔金构造带西段的榴辉岩呈透镜状产于长英质片麻岩中,它主要经历了进变质的角闪岩相(P=6.04-8.70Kb,T=615-690℃)、峰期的榴辉岩相(P>15Kb,T=700-850℃)及减压过程中的麻粒岩相(P=11-14Kb,T=750℃)及角闪岩相(P=6.3-9.5,T=619-738℃)的变质作用,构成一个顺时针的PT轨迹。

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这对开发者来说是一个非常大的挑战,尤其是需要不断变化的Ajax。