Fault configuration produced by initial arc rifting in the Parece Vela Basin as deduced from seismic reflection data

• Published in: The island arc Vol. 16; no. 3; pp. 338 - 347
• Main Authors: Yamashita, Mikiya, Tsuru, Tetsuro, Takahashi, Narumi, Takizawa, Kaoru, Kaneda, Yoshiyuki, Fujioka, Kantaro, Koda, Keita
• Format: Journal Article
• Language: English
• Published: Melbourne, Australia Blackwell Publishing Asia 01.09.2007
• Subjects: back-arc basin; Izu-Ogasawara Arc; Kyushu-Palau Ridge; Parece Vela Basin; pre-stack depth migration
• ISSN: 1038-4871; 1440-1738
• DOI: 10.1111/j.1440-1738.2007.00594.x

The Parece Vela Basin (PVB), which is a currently inactive back‐arc basin of the Philippine Sea Plate, was formed by separation between the Izu‐Ogasawara Arc (IOA) and the Kyushu‐Palau Ridge (KPR). Elucidating the marks of the past back‐arc opening and rifting is important for investigation of its crustal structure. To image its fault configurations and crustal deformation, pre‐stack depth migration to multichannel seismic reflection was applied and data obtained by the Japan Agency for Marine‐Earth Science and Technology and Metal Mining Agency of Japan and Japan National Oil Corporation (Japan Oil, Gas and Metals National Corporation). Salient results for the pre‐stack depth‐migrated sections are: (i) deep reflectors exist around the eastern margin of KPR and at the western margin of IOA down to 8 km depth; and (ii) normal fault zones distributed at the eastern margin of the KPR (Fault zone A) and the western margin of the IOA (Fault zone B) have a total displacement of greater than 500 m associated with synrift sediments. Additional normal faults (Fault zone C) exist 20 km east of the Fault zone B. They are covered with sediment, which indicates deposition of recent volcanic products in the IOA. According to those results: (i) the fault displacement of more than 500 m with respect to initial rifting was approximately asymmetric at 25 Ma based on PSDM profiles; and (ii) the faults had reactivated after 23 Ma, based on the age of deformed sediments obtained from past ocean drillings. The age of the base sediments corresponds to those of spreading and rotation after rifting in the PVB. Fault zone C is covered with thick and not deformed volcanogenic sediments from the IOA, which suggests that the fault is inactive.