• These NNE and ne faults become a long transform fault system and formed a boundary between the eastern margin of China Continental Plate and Philippine Sea Plate.

    这些北北东向和北东向断层形成一条巨长的转换断层系列,也是中国大陆板块东缘与菲律宾洋块的一条边界。

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  • The plate activity is weaker in the passive continental margin of the northern South China Sea, which is favorable for forming the large-scale gas field and gas hydrate reservoirs.

    南海北部被动大陆边缘是板块活动相对较弱的地区,业已证实是巨大天然气田形成的有利场所,同时也是水合物发育的有利地区。

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  • Southeastern China continental margin has undergone a complicated convergence process of the Eurasian plate with the Pacific plate and Tethys plate.

    中国大陆东、南边缘经历了欧亚板块与太平洋板块和特提斯板块会聚作用的复杂过程。

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  • This is apparently related to the tectonic setting of Shandong, namely, the continental margin where the Pacific Plate collided against the Eurasian Plate.

    之所以如此,显然与山东所处的大地构造位置,即太平洋板块与欧亚板块相互碰撞的陆缘地带密切相关。

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  • The major disruption of Machaoying-Panhe defines the active continental margin of the north China plate and the south margin of the Epicontinental Sea in the Paleozoic period.

    马超营一一潘河大断裂,界定了古生代时期华北板块活动大陆边缘陆架与陆缘表海的南部边沿。

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  • The major disruption of Heigou-Luanchuan has determined the active continental margin of the ancient north China plate.

    黑沟一栾川大断裂,限定了古华北板块南部活动大陆边缘的边界。

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  • There are various indications that the Liuling Group belongs to the stable continental margin deposits of the north of the Yangtse plate.

    冬种迹象表明,刘岭群应属扬子板块北部的稳定大陆边缘沉积。

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  • It is one of the evidences of the earliest plate subduction at the south margin of the ancient continental plate of North China.

    这是华北古大陆板块南部最早的板块俯冲活动的证据之一。

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  • Marine Meso-Paleozoic structures in the region have undergone three evolution stages of Pre-Yangzi Plate, stable platform and West Pacific active continental margin.

    江苏下扬子区的海相中—古生界构造演化经历了前扬子板块、稳定地台和西太平洋活动陆缘等三大阶段。

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  • The passive continental margin is a comparatively weak region of plate tectonic movement, but it is a favorable region for gas hydrate.

    非活动陆缘是板块活动相对较弱的地区,也是水合物发育的有利地区。

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  • The passive continental margin is a comparatively weak region of plate tectonic movement, but it is a favorable region for gas hydrate.

    非活动陆缘是板块活动相对较弱的地区,也是水合物发育的有利地区。

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