Skip to main content

and
  1. No Access

    Article

    The Cenozoic activities of Yangjiang-Yitongdong Fault: insights from analysis of the tectonic characteristics and evolution processes in western Zhujiang (Pearl) River Mouth Basin

    The Yangjiang-Yitongdong Fault (YJF) is an important NW-trending regional fault, which divides the Zhujiang (Pearl) River Mouth Basin (ZRMB) into western and eastern segments. In Cenozoic, the northern contine...

    Yuhan Li, Rongwei Zhu, Hailing Liu, Xuelin Qiu, Haibo Huang in Acta Oceanologica Sinica (2019)

  2. No Access

    Article

    Relocation of two earthquakes in the Southwest Indian Ridge area combining land seismic stations’ with OBSs’ data

    Two earthquakes were recorded by 20 ocean bottom seismometers (OBS) deployed in the Southwest Indian Ridge (SWIR) area during a three-dimensional seismic survey in 2010. Their magnitudes (both M ...

    Wei Luo, Minghui Zhao, Jiazheng Zhang, Chunhui Tao in Marine Geophysical Research (2017)

  3. No Access

    Article

    The role of rifting in the development of the continental margins of the southwest subbasin, South China Sea: Insights from an OBS experiment

    The continental margins of the southwest subbasin in the South China Sea mark a unique transition from multi-stages magma-poor continental rifting to seafloor spreading. We used reflection and refraction profi...

    Chuanchuan Lü, Tianyao Hao, Jian Lin, Xuelin Qiu in Marine Geophysical Research (2017)

  4. No Access

    Article

    Segmentation of the Manila subduction system from migrated multichannel seismics and wedge taper analysis

    Based on bathymetric data and multichannel seismic data, the Manila subduction system is divided into three segments, the North Luzon segment, the seamount chain segment and the West Luzon segment starts in So...

    Junjiang Zhu, Zongxun Sun, Heidrun Kopp, Xuelin Qiu in Marine Geophysical Research (2013)

  5. No Access

    Article

    Seismic phases from the Moho and its implication on the ultraslow spreading ridge

    The Moho interface provides critical evidence for crustal thickness and the mode of oceanic crust accretion. The seismic Moho interface has not been identified yet at the magma-rich segments (46°–52°E) of the ...

    Jiazheng Zhang, Minghui Zhao, Xuelin Qiu, Jiabiao Li in Acta Oceanologica Sinica (2013)