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- W2015965132 abstract "Luzon is part of the Taiwan-Luzon-Mindoro mobile belt which marks the plate boundary between the Eurasian and Philippine Sea plates. On Luzon, the Philippine Fault runs parallel to the Philippine archipelago for more than 1300 km, and is an active, left-lateral, strike-slip fault which forms a braided system. Detailed field mapping together with structural and biostratigraphic analysis have been conducted in the Ilocos Foothills, on the western flank of the Central Cordillera Cenozoic magmatic arc. This area, on the northwestern tip of Luzon, appears to consist of three large tectonic units which are continuous for more than 200 km and bounded by major left-lateral strike-slip faults related to the Philippine Fault. From west to east these units are as follows: (1) the Vigan-Laoag Coastal Strip (VLCS) consists of an ultramafic basement which is strongly tectonized and unconformably overlain by a relatively undeformed Middle Miocene to Pliocene sedimentary cover. (2) The Vintar Median Strip (VMS) is bounded to the west by the Vigan-Aggao wrench fault which upthrusts westwards, and to the east by the Abra River strike-slip fault. This unit is composed of a thick (6–10 km) Late Eocene to Pliocene volcaniclastic sequence deposited in a basin which was fed mainly by the Central Cordillera but also, until the early Miocene, by an ultramafic high composed of the VLCS basement; this sequence is strongly folded. (3) The Eastern Strip (ES) is a Late Eocene to Miocene volcaniclastic sequence intruded by Oligocene and Miocene rocks. This structural pattern results from two major tectonic episodes: (1) The late Middle to Late Miocene episode comprises the Abra River strike-slip faulting. This is characterized by the folding of a 20 km wide band and by the creation of a ridge (transverse to the tectonic strips) related to the Abra River Fault restraining bend. This ridge seems to have absorbed the compressive deformation, whereas the strike-slip component was accommodated by the nearly pure strike-slip faulting along the Abra River Fault. (2) The Pliocene(?) to Quaternary episode involved strike-slip activity propagating westward from the Abra River Fault (relatively inactive during this phase) to the Vigan-Aggao wrench fault." @default.
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- W2015965132 date "1990-11-01" @default.
- W2015965132 modified "2023-10-07" @default.
- W2015965132 title "The Philippine wrench fault system in the Ilocos Foothills, northwestern Luzon, Philippines" @default.
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- W2015965132 doi "https://doi.org/10.1016/0040-1951(90)90417-7" @default.
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