Ophiolite complexes as collision zone markers: making the case for the Antique Ophiolite Complex, Panay Island, central Philippines
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引用本文:G.P. YUMUL Jr.,R.A. TAMAYO Jr.,C.B. DIMALANTA.2009.Ophiolite complexes as collision zone markers: making the case for the Antique Ophiolite Complex, Panay Island, central Philippines[J].地球学报,30(S1):91.
DOI:10.3975/cagsb.2009.s1.36
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作者单位E-mail
G.P. YUMUL Jr. National Institute of Geological Sciences, College of Science, University of the Philippines
Department of Science and Technology, Bicutan, Taguig City, Metro Manila, Philippines 
gpyumul@dost.gov.ph/csrwg@yahoo.com 
R.A. TAMAYO Jr. National Institute of Geological Sciences, College of Science, University of the Philippines  
C.B. DIMALANTA National Institute of Geological Sciences, College of Science, University of the Philippines  
中文摘要:The collision between the North Palawan Block (NPB) and Philippine Mobile Belt (PMB) has been the subject of studies considering its significance in help-ing define the tectonic evolution of the Philippine is-land arc system. The geology of the western Panay island reveals the presence of a continent-related block (Buruanga Peninsula) juxtaposed to an oceanic frag-ment (Antique Ophiolite Complex). Our recent work in the Buruanga Peninsula helped us define the terrane boundary between the Peninsula and the Antique Ophiolite Complex. However, considering available published data, the Antique Ophiolite Complex has never been considered to be a part of the NPB and to mark the collision zone between Palawan and the PMB.
中文关键词:North Palawan Block  Philippine Mobile Belt  Antique Ophiolite Complex
 
Ophiolite complexes as collision zone markers: making the case for the Antique Ophiolite Complex, Panay Island, central Philippines
Abstract:The collision between the North Palawan Block (NPB) and Philippine Mobile Belt (PMB) has been the subject of studies considering its significance in help-ing define the tectonic evolution of the Philippine is-land arc system. The geology of the western Panay island reveals the presence of a continent-related block (Buruanga Peninsula) juxtaposed to an oceanic frag-ment (Antique Ophiolite Complex). Our recent work in the Buruanga Peninsula helped us define the terrane boundary between the Peninsula and the Antique Ophiolite Complex. However, considering available published data, the Antique Ophiolite Complex has never been considered to be a part of the NPB and to mark the collision zone between Palawan and the PMB.
keywords:North Palawan Block  Philippine Mobile Belt  Antique Ophiolite Complex
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