- 更多网络例句与俯冲断层的相关的网络例句 [注：此内容来源于网络，仅供参考]
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This type of faulting is common in areas of compression, such as regions where one plate is being subducted under another as in Japan.
这种类型的断层通常出现在挤压区域，比如像日本那样的，板块向另一板块之下俯冲的区域。
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Firstly, based on the distribution of global earthquakes and their kinematic and dynamic characteristics, the most active global-scale tectonics can be divided into three first-order tectonic system: the circum-Pacific deep subduction tectonic system, which is the region that oceanic lithosphere subduct under continental lithosphere; the mid-oceanic ridge tectonic system, where the joint tectonics of rift valleys and transform faults distribute widely; and the continent-continent shallow underthrusting tectonic system, where the different kinds of continental faults affect each other.
其中，环太平洋构造系以大洋岩石圈向大陆岩石圈俯冲为构造特征；大洋中脊构造系以大洋岩石圈内裂谷-转换断层的组合构造为特征；大陆构造系则以大陆岩石圈的边缘和内部各种断裂的相互作用为特征。
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The main study areas of SEIZE include:(1)physical nature of asperity;(2)temporal relationships among stress, strain, and pore fluid pressure throughout the earthquake cycle;(3)controls on the updip and downdip limits of the seismogenic zone of subduction thrusts;(4)nature of tsunamigenic earthquake zones;(5)role of large thrust earthquake in mass flux.
SEIZE的主要研究内容包括：①凸凹体的物理性质；②在地震周期里，应力、应变和孔隙流体成分随时间的变化；③在俯冲逆冲断层上，发震带上界和下界的确定；④引起海啸的发震带的特征；⑤大型逆冲带地震在物质转换过程中所起的作用。
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By analysing the molasse sediment, tectonic stress field, thrust fault system and comparing them with volcanic rocks and granites in the region, it is showed that Dabie orogenic belt had a strong intracontinental orogenesis whose deep dynamic processes were controlled by subduction with delamination during late stage of Cretaceous period-late Cretaceous period.
磨拉石沉积、构造应力场、逆冲断层系统和区域火山岩、花岗岩的综合分析表明，大别造山带早白垩世晚期—晚白垩世存在一次强烈的陆内造山作用，其深部动力学过程受控于拆沉中的俯冲作用。
- 更多网络解释与俯冲断层的相关的网络解释 [注：此内容来源于网络，仅供参考]
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subduction zone：消减带
而且进一步把这种在中、新生代以来的构造格式俯冲和仰冲本是冲断层两盘的相对位移运动.从地质力学看来,就是剪切作用的构造表现.可是现在很多板块构造学家却只强调俯冲,把与俯冲相当的大规模构造称为消减带(subduction zone)又称为贝尼霍夫带(Benioff zone),
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subduction：潜没
这种情况的断层就被称为逆冲断层(thrust fault),也有说法是'大逆冲',往往指的是断层面的角度接近水平程度. 这种断层一般发生在板块交界的地点,是大型快体的消减,潜没(subduction)带,即一个板块俯冲到另一个板块之下,逐渐消减的地区.