Age and tectonic evolution of the northwest corner of the West Philippine Basin

NCUIR > Research Center > Center for Environmental Studies > journal & Dissertation > Item 987654321/108656

Please use this identifier to cite or link to this item: https://ir.lib.ncu.edu.tw/handle/987654321/108656

Title:	Age and tectonic evolution of the northwest corner of the West Philippine Basin
Authors:	杜文斌;Doo, Wen-Bin;Hsu, Shu-Kun;Yeh, Yi-Ching;Tsai, Ching-Hui;Chang, Ching-Ming
Contributors:	環境研究中心
Keywords:	Bathymetry;Continental margins;Earth and Environmental Science;Earth Sciences;Geological time;Geophysics/Geodesy;Magma;Ocean floor;Oceanic crust;Oceanography;Offshore Engineering;Original Research Paper;Plate tectonics;Seafloor spreading;Seamounts;Seismology
Date:	2015-09-24
Issue Date:	2026-04-23 15:00:39 (UTC+8)
Publisher:	Springer Netherlands;Dordrecht: Springer Science and Business Media LLC
Abstract:	摘要： To understand the tectonic characteristics and age of the northwestern part of the West Philippine Basin (WPB), multi-beam bathymetry and geomagnetic data have been collected and analyzed. The seafloor morphology obviously shows NW–SE trending seafloor fabrics and NE–SW trending fracture zones, indicating a NE–SW seafloor spreading direction. An overlapping spreading center near 22°20′N and 125°E is identified. Besides, numerous seamounts indicate an excess supply of magma during or after the oceanic crust formation. A V-shaped seamount chain near 21°52′N and 124°26′E indicates a southeastward magma propagation and also indicates the location of the seafloor spreading ridge. On the basis of the newly collected geomagnetic data, the magnetic anomaly shows NW–SE trending magnetic lineations. Both bathymetry and geomagnetic data reveal NE–SW seafloor spreading features between the Gagua Ridge and the Luzon Okinawa fracture zone (LOFZ). Our magnetic age modeling indicates that the age of the northwestern corner of the WPB west of the LOFZ is between 47.5 to 54 Ma (without including overlapping spreading center), which is linked to the first spreading phase of the WPB to the east of the LOFZ. In addition, the age of the Huatung Basin is identified to be between 33 to 42 Ma, which is similar to the second spreading phase of the WPB. 其他題名： Mar Geophys Res 出版者： Dordrecht: Springer Science and Business Media LLC 出版日期： 2015-09-01 出處： Marine Geophysical Research, 2015-09, Vol.36 (2), p.113-125 資源來源： SpringerLink Journals - AutoHoldings 版權： Springer Science+Business Media Dordrecht 2014 版權： Springer Science+Business Media Dordrecht 2015 識別號： ISSN: 0025-3235 識別號： EISSN: 1573-0581 識別號： DOI: 10.1007/s11001-014-9234-8
Appears in Collections:	[Center for Environmental Studies] journal & Dissertation

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