Just Earthquakes. It is more obvious on seismic and aeromagnetic data than the northern part of the known Philippine fault and thus may have accommodated more motion.We have made a preliminary evaluation of the total slip on the Sibuyan Sea branch by attempting to restore long-wavelength geophysical and geologic features, including forearc basins, ophiolite belts, volcanic belts, and regional Bouguer, free-air and magnetic anomalies, which suggests the possibility of 200–300 km of slip since about the early or middle Miocene.
The Sibuyan Sea The earthquake, tectonic in origin, had the following intensities: Intensity V- Lignon Hill, Legaspi Intensity IV-Masbate City, Sorsogon City, Irosin, Sorsogon and Sto. The MUSASHI, the second of two Yamato-class battleships, shared the honor with the lead ship YAMATO as the largest battleship ever constructed in naval history. It is bounded by the island of Panay to the south, Mindoro to the west, Masbate to the east, and to the north Marinduque and the Bicol Peninsula of Luzon Island. It is bounded by the island of Panay to the south, Mindoro to the west, Masbate to the east, and to the north Marinduque and the Bicol Peninsula of Luzon Island. This paper outlines evidence from these surveys for a previously unrecognized major branch of the Philippine fault system and tentatively discusses its paleogeographic implications.We have interpreted aeromagnetic data covering most of the length of the fault and seismic profiles crossing it at various locations.
The Philippine fault is one of the major strike-slip faults of the world, extending over 1200 km from the Lingayen-La Union region of northwestern Luzon to the Davao Gulf south of Mindanao.
Surprisingly, the data also show a major, previously unrecognized, branch of the Philippine fault, here named the Sibuyan Sea branch. By continuing you agree to the.Copyright © 2020 Elsevier B.V. or its licensors or contributors.ScienceDirect ® is a registered trademark of Elsevier B.V.A new branch of the Philippine fault system as observed from aeromagnetic and seismic data.Copyright © 1990 Published by Elsevier B.V.https://doi.org/10.1016/0040-1951(90)90419-9. It is bounded by the island of Panay to the south, Mindoro to the west, Masbate to the east, and to the north Marinduque and the Bicol Peninsula of Luzon Island..
A number of other active intra-arc fault systems are associated with high seismic activity, including the Cotabato Fault and the Verde Passage-Sibuyan Sea Fault (Galgana et al., 2007). After collision with the Palawan-Mindoro continental block, continued motion along the Manila trench north of Mindoro has ruptured the central Philippines along the Sibuyan Sea branch of the Philippine fault. Cotabato Fault and the Verde Passage-Sibuyan Sea Fault (Galgana et al., 2007). The Sibuyan Sea branch is 350 km long and is presently active. The Sibuyan Sea is a small sea in the Philippines that separates the Visayas from the northern Philippine island of Luzon. The Sibuyan Sea branch is 350 km long and is presently active.
6). The Sibuyan Sea is connected to the Sulu Sea via the Tablas Strait in the west, the South China Sea via the Isla Verde Passage in the northwest, and the Visayan Sea via the Jintotolo Channel in the south-east. The Island Arc 9.Besana, G.M., Ando, M., 2005.
Sibuyan Sea branch of the Philippine fault Aeromagnetic mapping through the northeast- ern margin of the Sibuyan Sea and Tayabas Bay produces a very obvious and previously unrecog- nized linear anomaly that is similar in character to the magnetic expression of the known Philippine fault zone but, if anything, is better displayed in the magnetic data (Fig.
A review of the seismicity along the Masbate segment of the Philippine Fault and the Sibuyan Sea fault is presented in light of the two damaging earthquakes of 15 February 2003.
The Philippine fault is well displayed in the aeromagnetic data.
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