热带海洋学报 ›› 2017, Vol. 36 ›› Issue (3): 1-19.doi: 10.11978/2016092CSTR: 32234.14.2016092
• • 下一篇
收稿日期:
2016-09-30
修回日期:
2016-12-21
出版日期:
2017-05-20
发布日期:
2017-06-01
作者简介:
作者简介:周蒂(1944—), 女, 博士, 研究员。主要从事海洋地质与模拟研究。E-mail:
基金资助:
Received:
2016-09-30
Revised:
2016-12-21
Online:
2017-05-20
Published:
2017-06-01
Supported by:
摘要:
晚中生代以来太平洋构造域的地质过程明显影响了东亚陆缘的构造演化、岩浆活动和成矿过程, 加强对太平洋板块自身演化过程的认识是我们正确理解东亚陆缘构造变迁的基础。文章从太平洋域与特提斯域地质过程对比、古太平洋演化的重要事件和扩张脊俯冲三个方面简要介绍古—今太平洋的构造演化的研究成果, 特别是最新成果, 分析晚中生代以来太平洋域构造演化对东亚陆缘的可能影响, 以期引起学界对开展有关洋陆结合研究的重视, 并提供一份快速参考资料。
周蒂, 孙珍. 晚中生代以来太平洋域板块过程及其对东亚陆缘构造研究的启示[J]. 热带海洋学报, 2017, 36(3): 1-19.
Di ZHOU, Zhen SUN. Plate evolution in the Pacific domain since Late Mesozoic and its inspiration to tectonic research of East Asia margin[J]. Journal of Tropical Oceanography, 2017, 36(3): 1-19.
图9
105~100Ma板块回溯图, 显示当时的主要构造事件[译自Matthews等(2012)]^a. 东冈瓦纳区域; b. 大西洋区域。红/橙色箭头分别表示前/后板块运动方向(不按比例); 齿线表示俯冲带, 其中红色段表示当时终止活动的东冈瓦纳俯冲带; 五角星表示布韦(Bouvet)地幔柱位置; 浅灰和深灰色块分别表示陆地和大陆架; 粉色块表示大火山岩省; 横线阴影表示后来被俯冲掉的洋底。S: 海底扩张开始处; CE: 挤压事件发生处; CaP: 卡特奎尔(Catequil)板块; ChP: 查兹卡(Chazca)板块; HP: 希库朗伊(Hikurangi)板块; IB: 伊比利亚(Iberian)板块; JP: 江可申(Junction)板块; MP: 马尼希基(Manihiki)板块"
图10
早始新世事件在太平洋及邻域的表现[自Seton等(2015)]^1. 澳大利亚—南极扩张方向改变(53~50Ma); 2. 塔斯曼、珊瑚海扩张停止(52Ma); 3. 南太平洋三联点重组(50~48Ma); 4. 法拉隆板块再分裂, 温哥华板块形成成(53Ma); 5. 库拉板块扩张方向由SN变为NW—SE (53Ma)和停止扩张(41Ma); 6. 伊豆—小笠原—马里亚纳火山弧开始形成(51~48Ma); 7. 沿汤加—克马德克火山弧的俯冲开始; 8. 夏威夷—皇帝岛链转折及太平洋漂移方向45°逆时针旋转(53~47Ma)。图中黑色粗线表示洋中脊; 红色齿线表示俯冲带; 浅黄色表示陆地; 浅蓝色表示海洋; 深蓝线表示转换断层; 紫色表示火山岛"
图12
依扎奈崎—太平洋扩张脊俯冲模式图^a和b: 白垩纪近垂直俯冲模式。白垩纪时扩张脊与海沟近垂直地俯冲, 且三联点向北东位移(Maruyama et al, 1997)。黄色箭头及其标示: 板块运动方向及其速率。c: 早古近纪近平行俯冲模式。早古近纪时扩张脊与海沟近平行地俯冲(Seton et al, 2012); IZA: 依扎奈崎板块; PAC: 太平洋板块; JUN: 江可申板块; LHR: 豪勋爵隆起板块; 黑色箭头表示板块运动方向。d: 早白垩世斜交俯冲模式。早白垩世时扩张脊向下扬子地块俯冲, 与海沟大角度相交(Ling et al, 2009); 黑色箭头表示板块运动方向"
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