弧后盆地

喀喇昆仑地区早二叠世弧后盆地

Early Permian back arc basin in the Karakorum Mountains

冲绳海槽仍是一个软流圈在汇聚的弧后盆地。

The Okinawa Trough is a back arc basin still driven by the converging asthenosphere .

微量元素主要显示MORB的特征，部分判别图显示MORB和岛弧拉斑玄武岩（IAT）的过渡特征，推测可能产于弧后盆地环境。

The trace elements main manifestation MORB characteristic , manifestation MORB and IAT transition characteristic in the part differentiate diagram , guess may generate from back-arc basin environment .

同时存在岛弧型和MORB型两种熔岩，可能是弧后盆地（特别是早期扩张弧后盆地）岩浆作用的一个共同属性。

During the earlier stage of evolution , there coexist the two MORB-like and ARC-like lavas , it may be the nature of the magma in back arc basins ( especially in the earlier stage ) .

沉积于中中新世到上新世的浊积砂体是第三纪Niigata弧后盆地的主要油气储层之一，该盆地是日本列岛最富产石油的盆地。

Many turbidite sandstone bodies , deposited during the Middle Miocene to Pliocene , are distributed and form one of major reservoirs for oil and gas in the Tertiary Niigata backarc sedimentary basin , the most productive oil basin in the Japanese Islands .

论海沟岛弧弧后盆地复合体系的形成机制

On the formation mechanism of trench arc back arc basic system

早侏罗世由弧后盆地向前陆盆地转化。

During Cretaceous and Quaternary it changed into the mountain front basin .

马里亚纳海槽是一个正在扩张的弧后盆地。

The Mariana Trough is an active spreading back-arc basin .

准噶尔弧后盆地与弧后残余盆地

On the Junggar back-arc basin and back-arc relict basins

残留弧后盆地及其辨识准则和实例

Relict back-arc basins : principles of recognition and possible new examples from China

裂陷作用也控制着弧后盆地的形成。

Rifting played an important role in formation of the back arc basins .

竟柱山组沉积-火山岩的形成环境揭示了比如盆地的性质在晚白垩世已由弧后盆地转换为前陆盆地。

The Biru Basin developed into a foreland basin during the Late Cretaceous .

右江弧后盆地的关闭经历了突变式回返褶皱和渐变隆起上升两种不同的构造作用。

The closure ofYoujiang back-arc basin went through abrupt inversing-folding and gradual uplifting .

晚奥陶世北秦岭弧后盆地放射虫组合

The Late Ordovician Radiolarian Assemblage of the North Qinling Back-arc Basin , China

北祁连山早古生代洋脊-洋岛和弧后盆地火山作用

Post-ALL Early Palaeozoic Mid-Ocean Ridge-Ocean Island and Back-Arc Basin Volcanism in the North Qilian Mountains

俯冲带和弧后盆地；

Subduction zone and back arc basins ;

西地中海的弧后盆地

The back-arc basins in the western Mediterranean

弧后盆地的形成与演化探讨&以东亚陆缘区为例

Exploration on the formation and evolution of back-arc basins-example of continental margins in East Asia

弧后盆地扩张到达小洋盆，出现蛇绿混杂岩。

The small ocean basin is formed and the ophiolite appear when back arc basin expands .

论西太平洋活动大陆边缘中-新生代弧后盆地的分类和演化

On the generation and evolution of Mesozoic Cenozoic back arc basins of Western Pacific active continental margin

弧后盆地层序地层研究

Sequence stratigraphy of retroarc basin

热液区主要分布在大洋中脊、弧后盆地和热点区。

The hydrothermal area distributes mostly at the mid ocean ridge , back arc basin and hot spot .

晚二叠世末，该地区变成弧后盆地，进一步转化成前陆盆地。

The late Permian it was changed into the back arc basin , and transformed into foreland basin .

弧后盆地发育多套砂泥（页）岩互层的储盖组合，具有良好的储集条件和封盖条件。

There are several sets of reservoir and cap combination in back-arc basin with good reservoir and capping capability .

综合分析，本区在中泥盆世处于汇聚板块一侧的岛弧及弧后盆地。

This area was in an arc and rear - arc basin on convergent plates in the Middle Devonian .

冲绳海槽火山岩&揭示弧后盆地早期扩张动力学过程的钥匙

Volcanic rocks from Okinawa TROUGH-A key to the dynamic process during the initial spreading stage of the back arc basin

蛇绿混杂岩中的北部中-酸性火山岩和南部蛇绿岩分别代表了弧后盆地扩张开裂早期和晚期阶段的产物。

Volcanic-sedimentary assemblage of the northern melange was formed in the early stage of the expanding of the back-arc basin .

准噶尔盆地是由准噶尔及吐鲁番、哈密地区石炭纪弧后盆地未完全关闭演化而来的二叠纪-侏罗纪弧后残余盆地组成。

The Junggar Basin consists of the Permian-Jurassic back-arc relict basins as the survival of the Carboniferous unfinished closure back-arc basins .

北秦岭弧后盆地俯冲消减与陆壳物质再循环&桃园岩体和黄岗杂岩体的地球化学证据

Subduction of back-arc basin and recycling of crustal substance in northern qinling : geochemical evidence of Taoyuan intrusion and Huanggang intrusive complex

从弧后盆地到前陆盆地北祁连造山带奥陶纪泥盆纪的沉积盆地与构造演化

From the back - arc basin to foreland basin - Ordovician-Devonian sedimentary basin and tectonic evolution in the North Qilian orogenic belt