THE PETROLEUM POTENTIAL OF DEEP-WATER NORTHWEST PALAWAN BLOCK GSEC-66

Citation
Ao. Sales et al., THE PETROLEUM POTENTIAL OF DEEP-WATER NORTHWEST PALAWAN BLOCK GSEC-66, Journal of Asian earth sciences, 15(2-3), 1997, pp. 217-240
Citations number
16
Categorie Soggetti
Geosciences, Interdisciplinary
Volume
15
Issue
2-3
Year of publication
1997
Pages
217 - 240
Database
ISI
SICI code
Abstract
This paper presents the results of the evaluation of the petroleum pot ential of the deep-water acreage of Philodrill, GSEC 66, or what the a uthors call the ''Northwest Malampaya Block''. All the elements necess ary for a major hydrocarbon accumulation are believed to be present in the block. Probable source rocks are the deep-water Nido Limestone, t he pre-Nido Early Tertiary syn-rift section, and pre-Tertiary sediment s. Potential reservoirs include the Nido reefal buildups, Nido and pre -Nido detrital and/or fractured carbonates, Early Miocene Galoc elasti c equivalent turbidites and pre-Nido sediments. The principal play-typ es recognized in the area are the Late Oligocene to Early Miocene reef s and the erosional/karsted carbonate highs. After evaluation of avail able pre-1982 seismic data, an acquisition program of 1625 km was unde rtaken. Eleven leads/prospects were delineated in the area after the i nterpretation of this new seismic data. Two prospects were upgraded to drillable status (the Santa Monica Prospect and the Ipil Prospect). T he Santa Monica Prospect is a well-defined four way dip closure on the Nido Limestone with a vertical closure of over 1500 feet and an areal closure of over 20,500 acres. The Ipil Prospect is a gently closed fe ature developed at the Nido Limestone platform level with an areal clo sure of over 11,600 acres and a vertical relief of 400 feet. The techn ical merits of the delineated huge prospects, combined with the very f avorable deep-water exploration terms of the Philippines and their pro ximity to the soon-to-be-developed Malampaya-Camago Field, make this b lock a very promising area for further exploration work. (C) 1997 Publ ished by Elsevier Science Ltd.