The Zambales complex: gravity anomalies and a very strange ophiolite
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引用本文:John MILSOM,Jenny BARRETTO,Jonathan AITCHISON.2009.The Zambales complex: gravity anomalies and a very strange ophiolite[J].地球学报,30(S1):37.
DOI:10.3975/cagsb.2009.s1.21
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作者单位E-mail
John MILSOM Department of Earth Sciences, University of Hong Kong, Pokfulam Rd, Hong Kong, China gladassoc@btinternet.com 
Jenny BARRETTO Planades Foundation, University of the Philippines, Diliman, Metro Manila  
Jonathan AITCHISON Department of Earth Sciences, University of Hong Kong, Pokfulam Rd, Hong Kong, China  
中文摘要:In common with most of the larger ophiolite bodies that were emplaced during the Cenozoic and late Mesozoic and which have experienced relatively little post-emplacement disruption or metamorphism, the Zambales Ophiolite Complex (ZOC) of western Luzon (northern Philippines) is associated with very large gravity anomalies. Worldwide and in the ZOC, peak to trough amplitudes of more than 100 mGal are common and amplitudes in excess of 200 mGal are not unknown
 
The Zambales complex: gravity anomalies and a very strange ophiolite
Abstract:In common with most of the larger ophiolite bodies that were emplaced during the Cenozoic and late Mesozoic and which have experienced relatively little post-emplacement disruption or metamorphism, the Zambales Ophiolite Complex (ZOC) of western Luzon (northern Philippines) is associated with very large gravity anomalies. Worldwide and in the ZOC, peak to trough amplitudes of more than 100 mGal are common and amplitudes in excess of 200 mGal are not unknown
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