Earthquake Scenarios for Greater Metro Manila Area
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Extinguishment of Agency General Condition Revocation Withdrawal Of
Extinguishment of Agency General condition Revocation Withdrawal of agent Death of the Principal Death of the Agent CASES Republic of the Philippines SUPREME COURT Manila FIRST DIVISION G.R. No. L-36585 July 16, 1984 MARIANO DIOLOSA and ALEGRIA VILLANUEVA-DIOLOSA, petitioners, vs. THE HON. COURT OF APPEALS, and QUIRINO BATERNA (As owner and proprietor of QUIN BATERNA REALTY), respondents. Enrique L. Soriano for petitioners. Domingo Laurea for private respondent. RELOVA, J.: Appeal by certiorari from a decision of the then Court of Appeals ordering herein petitioners to pay private respondent "the sum of P10,000.00 as damages and the sum of P2,000.00 as attorney's fees, and the costs." This case originated in the then Court of First Instance of Iloilo where private respondents instituted a case of recovery of unpaid commission against petitioners over some of the lots subject of an agency agreement that were not sold. Said complaint, docketed as Civil Case No. 7864 and entitled: "Quirino Baterna vs. Mariano Diolosa and Alegria Villanueva-Diolosa", was dismissed by the trial court after hearing. Thereafter, private respondent elevated the case to respondent court whose decision is the subject of the present petition. The parties — petitioners and respondents-agree on the findings of facts made by respondent court which are based largely on the pre-trial order of the trial court, as follows: PRE-TRIAL ORDER When this case was called for a pre-trial conference today, the plaintiff, assisted by Atty. Domingo Laurea, appeared and the defendants, assisted by Atty. Enrique Soriano, also appeared. A. -
Geochemistry and Tectonic Setting of the Luzon Arc, Philippines
Geochemistry and tectonic setting of the Luzon arc, Philippines MARC J. DEFANT Department of Geology, University of South Florida, Tampa, Florida 33620 RENE^C^^AUR^Y } laboratoire de Petrologie et G. S. Oceanologie et Geodynamique, Universite de Bretagne Occidentale, 29287 Brest, France JELLE DE BOER Department of Earth and Environmental Sciences, Wesleyan University, Middletown, Connecticut 06457 JEAN-LOUIS JORON Groupe des Sciences de la Terre, Laboratoire Pierre Siie, Centre d'Etudes Nucléaires de Saclay, B.P. 2, 91191 Gif sur Yvette, France ABSTRACT ment) with the Manila Trench. In contrast, unreported analytical data, along the entire ex- Babuyan segment samples (north) have un- tent of the Luzon arc and to discuss possible Miocene (10 Ma) to Recent volcanism is usual island-arc Nd and Sr isotopic ratios that origins of these compositional variations. associated with eastward subduction along fall below the mantle array; they appear to be the Manila Trench for some 1,200 km from the result of sediment source contaminants or GEOLOGIC SETTING the Coastal Range in Taiwan south to Min- a unique mantle composition. Incorporation doro. We suggest calling this the "Luzon of sediments analyzed from eastern China Tectonic Framework arc." There are five distinct segments along and Taiwan into a MORB-type mantle can this arc: Mindoro, Bataan, Northern Luzon, explain the Nd and Sr isotopic ratios of the The Manila Trench is a broadly arcuate Babuyan, and Taiwan. The Bataan and Min- Babuyan segment. (concave eastward) structure, which extends doro segments in the south are separated by a from about 13° to 21° N (Figs. -
Philippine Island Arc System Tectonic Features Inferred from Magnetic Data Analysis
Terr. Atmos. Ocean. Sci., Vol. 26, No. 6, 679-686, December 2015 doi: 10.3319/TAO.2015.05.11.04(TC) Philippine Island Arc System Tectonic Features Inferred from Magnetic Data Analysis Wen-Bin Doo1, *, Shu-Kun Hsu1, 2, and Leo Armada 2 1 Center for Environmental Studies, National Central University, Taoyuan City, Taiwan, R.O.C. 2 Department of Earth Sciences, National Central University, Taoyuan City, Taiwan, R.O.C. Received 18 February 2013, revised 22 November 2013, accepted 11 May 2015 ABSTRACT Running along the middle of the Philippine archipelago from south to north, the Philippine fault zone is one of the world’s major strike-slip faults. Intense volcanism in the archipelago is attributed to the ongoing subduction along the trench systems surrounding it. This study interprets the magnetic data covering the Philippine fault zone and the bounding archi- pelago subduction systems to understand the structural characteristics of the study area. Magnetic data analysis suggests that the Philippine fault is roughly distributed along the boundary of high/low magnetization and separates the different amplitude features of the first order analytic signal. Visayas province is a specific area bounded by the other parts of the Philippine ar- chipelago. Further differentiating the tectonic units, the proto-Southeast Bohol Trench should be the main tectonic boundary between Visayas and Mindanao. A clear NE - SW boundary separates Luzon from Visayas as shown by the variant depths to the top of the magnetic basement. This boundary could suggest the different tectonic characteristics of the two regions. Key words: Philippine fault, Philippine archipelago, Magnetic data, Tectonic Citation: Doo, W. -
Evaluating the Seismic Hazards in Metro Manila, Philippines
EVALUATING THE SEISMIC HAZARDS IN METRO MANILA, PHILIPPINES Ivan Wong1, Timothy Dawson2, and Mark Dober3 1 Principal Seismologist/Vice President, Seismic Hazards Group, URS Corporation, Oakland, California, USA 2 Project Seismic Geologist, Seismic Hazards Group, URS Corporation, Oakland, California, USA 3 Senior Staff Seismologist, Seismic Hazards Group, URS Corporation, Oakland, California, USA Email: [email protected] ABSTRACT: We have performed site-specific probabilistic seismic hazard analyses (PSHA) for four sites in the Manila metropolitan area. The Philippine Islands lie within a broad zone of deformation between the subducting Eurasian and Philippine Sea Plate. This deformation is manifested by a high level of seismicity, faulting, and volcanism. The Philippines fault zone is a major left-lateral strike-slip fault that remains offshore east of Manila. The Marikina Valley fault system (MVFS) is the closest active fault to Manila and represents the most likely near-field source of large damaging earthquakes. The largest earthquake that has struck Manila historically, surface wave magnitude (MS) 7.5, occurred in 1645. Manila has experienced other historical damaging earthquakes numerous times. We have included 14 crustal faults, and the Manila Trench, Philippines Trench, and East Luzon Trough subduction zones (both megathrusts and Wadati-Benioff zones) in our seismic source model. We also have accounted for background crustal seismicity through the use of an areal source zone and Gaussian smoothing. Very little paleoseismic data is available for crustal faults in the Philippines including the MVFS so we have included a large amount of epistemic uncertainty in the characterization of these faults using logic trees. New empirical ground motion predictive equations were used in the PSHA. -
25/03/13 Travelife Magazine's Suitcase Tales: Forever Barolo -- Lunch and Paolo Scavino Wines at Masseto
25/03/13 Travelife Magazine's Suitcase Tales: Forever Barolo -- lunch and Paolo Scavino wines at Masseto Condividi 0 Altro Blog successivo» Crea blog Entra www.travelifemagazine.com/2012/06/forever-barolo-lunch-with-paolo-scavino.html 1/40 25/03/13 Travelife Magazine's Suitcase Tales: Forever Barolo -- lunch and Paolo Scavino wines at Masseto SUBSCRIBE TO TRAVELIFE ONLINE S A T U R D A Y , J U N E 9 , 2 0 1 2 NOW Forever Barolo -- lunch and Paolo Scavino wines at Masseto 2 TRAVELIFE'S ULTIMATE FOOD ISSUE It was the perfect day for a long wine lunch as we'd just closed Travelife Magazine's June-July 2012 issue in time for release on June 15 and so it already felt like a weekend. In addition, the venue was Masseto, one of my favorite restaurants in Manila, and I was lunching with a couple of friends. On sale everywhere now The lunch was hosted by Jojo Madrid, one of the partners behind Premium Wine Exchange and Masseto, as well as a board member of Travelife Magazine and a good friend; and the guest of honor was Elisa Scavino, daughter and one of the two heiresses (along with her sister) to the Barolo TRAVELIFE Magazine winery Paolo Scavino in northwest Italy, a winery known for its modernist outlook in a pretty traditional industry. Travelife is one of Southeast Asia's leading travel and lifestyle publications. It also has a television show and an A LOCAL LEGEND online blog. Contact us via [email protected] View my complete profile CATCH THE DIPLOMATIC TRAVELIFE www.travelifemagazine.com/2012/06/forever-barolo-lunch-with-paolo-scavino.html 2/40 25/03/13 Travelife Magazine's Suitcase Tales: Forever Barolo -- lunch and Paolo Scavino wines at Masseto COLUMN EVERY SUNDAY IN BUSINESS MIRROR CONNECT WITH US ON FACEBOOK TRAVELIFE MAGAZINE The Paolo Scavino winery is named after the founder, Elisa's grandfather, who established the winery in 1921 in Castiglione Falleto, one of the towns in the Barolo region, near Alba, a place particularly noted for its white truffles. -
Seismic Tomography Constraints on Reconstructing
SEISMIC TOMOGRAPHY CONSTRAINTS ON RECONSTRUCTING THE PHILIPPINE SEA PLATE AND ITS MARGIN A Dissertation by LINA HANDAYANI Submitted to the Office of Graduate Studies of Texas A&M University in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY December 2004 Major Subject: Geophysics SEISMIC TOMOGRAPHY CONSTRAINTS ON RECONSTRUCTING THE PHILIPPINE SEA PLATE AND ITS MARGIN A Dissertation by LINA HANDAYANI Submitted to Texas A&M University in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY Approved as to style and content by: Thomas W. C. Hilde Mark E. Everett (Chair of Committee) (Member) Richard L. Gibson David W. Sparks (Member) (Member) William R. Bryant Richard L. Carlson (Member) (Head of Department) December 2004 Major Subject: Geophysics iii ABSTRACT Seismic Tomography Constraints on Reconstructing the Philippine Sea Plate and Its Margin. (December 2004) Lina Handayani, B.S., Institut Teknologi Bandung; M.S., Texas A&M University Chair of Advisory Committee: Dr. Thomas W.C. Hilde The Philippine Sea Plate has been surrounded by subduction zones throughout Cenozoic time due to the convergence of the Eurasian, Pacific and Indian-Australian plates. Existing Philippine Sea Plate reconstructions have been made based primarily on magnetic lineations produced by seafloor spreading, rock magnetism and geology of the Philippine Sea Plate. This dissertation employs seismic tomography model to constraint the reconstruction of the Philippine Sea Plate. Recent seismic tomography studies show the distribution of high velocity anomalies in the mantle of the Western Pacific, and that they represent subducted slabs. Using these recent tomography data, distribution maps of subducted slabs in the mantle beneath and surrounding the Philippine Sea Plate have been constructed which show that the mantle anomalies can be related to the various subduction zones bounding the Philippine Sea Plate. -
Tomographic Evidence for a Slab Tear Induced by Fossil Ridge Subduction at Manila Trench, South China Sea
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/271621809 Tomographic evidence for a slab tear induced by fossil ridge subduction at Manila Trench, South China Sea Article in International Geology Review · December 2014 DOI: 10.1080/00206814.2014.929054 CITATIONS READS 4 169 3 authors, including: Jianke Fan Chinese Academy of Sciences 2 PUBLICATIONS 4 CITATIONS SEE PROFILE All content following this page was uploaded by Jianke Fan on 23 November 2015. The user has requested enhancement of the downloaded file. All in-text references underlined in blue are added to the original document and are linked to publications on ResearchGate, letting you access and read them immediately. This article was downloaded by: [Institute of Oceanology] On: 14 May 2015, At: 18:10 Publisher: Taylor & Francis Informa Ltd Registered in England and Wales Registered Number: 1072954 Registered office: Mortimer House, 37-41 Mortimer Street, London W1T 3JH, UK International Geology Review Publication details, including instructions for authors and subscription information: http://www.tandfonline.com/loi/tigr20 Tomographic evidence for a slab tear induced by fossil ridge subduction at Manila Trench, South China Sea Jian-ke Fanab, Shi-guo Wuab & George Spencec a Key laboratory of Marine Geology and Environment, Chinese Academy of Sciences, Qingdao 266071, PR China b Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, PR China c School of Earth and Ocean Sciences, University of Victoria, -
Oblique Convergence Between Trench-Arc System
Acta Oceanographica Taiwanica No.32, PP. 45-53, 1TAB., 3 Figs., May, 1994 OBLIQUE CONVERGENCE BETWEEN TRENCH-ARC SYSTEM AND CONTINENT-IMPLICATIONS FOR THE FORMAT1ON OF THE SUBMARINE PHYSIOGRAPHY OFF SOUTHERN TAIWAN Ho-Shung Yu and Gwo-Shyh Song ABSTRACT The northern Manila Trench-Luzon Arc system and the juxtaposed Asian continental margin were successively deformed by collision which began at about 5 Ma ago and has been propagating southward at a rate of about 9cm/year. As a consequence, folding, thrusting and orogenic sedimentation related to the east-west compressive stress have deformed the Asian continental margin and the trench-arc system into the mountain range (Taiwan) which plunges southward into the sea. Off southern Taiwan the sea floor features several prominent alternating N-S trending linear ridges and troughs. Beginning about 5 Ma, the northern tip of the Manila Trench has been progressively filled, closed and uplifted from north to south and compressed into the deformation front buried west of Taiwan. The northern portion of the Manila accretionary prism together with the Asian continental margin were deformed into the Central Range and its southern extension of the submarine Hengchun Ridge which ends at about 21°N. The northern segment of the forearc basin of the North Luzon Trough was deformed into the Longitudinal Valley, serving as the boundary between the Eurasian and Philippine Sea plates. The southern extension of the Longitudinal valley is represented by the Southern Longitudinal Trough, Huatung Ridge and Taitung Trough which merge together as the North Luzon Trough south of 21°N. During the last 3 Ma, the volcanic islands north of Lutao-Lanbsu Ridge then collided with the accreted Asian continental margin, resulting in the formation of the Coastal Range, and the Lichi melange accreted into eastern Taiwan. -
April 17, 2020 SECURITIES and EXCHANGE COMMISSION Secretariat Building, PICC Complex, Roxas Boulevard, Pasay City, 1307 Re
April 17, 2020 SECURITIES AND EXCHANGE COMMISSION Secretariat Building, PICC Complex, Roxas Boulevard, Pasay City, 1307 Re: Notice of Postponement and New Schedule of the Annual Stockholders’ Meeting________________ Dear Sir or Madam: Roxas Holdings, Inc. (the “Company”), through the undersigned, would like to inform the Securities and Exchange Commission (the “Commission”) that the Annual Stockholders’ Meeting (“ASM”) of the Company originally scheduled on March 18, 2020 at the Turf Room, Manila Polo Club, McKinley Road, Forbes Park, Makati City, Metro Manila, was postponed due to the exigent conditions surrounding the spread of the corona virus disease (COVID-19). The Board of Directors made this decision and the same was immediately disclosed to the Commission in a letter dated March 12, 2020, which was filed with the Commission on the same day. The date of the Company’s ASM per its By-laws is every 2nd Wednesday of March of each year. In compliance to the requirement provided in Section 2 of the SEC Memorandum Circular No. 9, Series of 2020, the Board of Directors of the Company has decided to tentatively set the ASM to May 13, 2020 in the same venue provided above, subject to further directives from the National Government and this Honorable Commission on the appropriate actions which must be done to address the COVID-19 pandemic, especially on the regulation of any mass gathering, and restriction on the movement of persons. In this regard, a clarificatory letter was electronically sent to the Commission yesterday (through MSRD COVID19 [email protected]) and the Company is awaiting response to its query. -
Numerical Study of Potential Extreme Tsunami Hazard in South China Sea
Available online at www.sciencedirect.com ScienceDirect Procedia Engineering 126 ( 2015 ) 332 – 338 7th International Conference on Fluid Mechanics, ICFM7 Numerical study of potential extreme tsunami hazard in South China Sea Zhi-Yuan Rena, Hua Liua, * aMOE Key Laboratory of Hydrodynamics, School of NAOCE, Shanghai Jiao Tong University, Shanghai, 200240, China Abstract In recent one decade, after two extreme tsunamis have produced devastating damage around the Indian Ocean and Pacific Ocean, it is necessary to investigate the tsunami hazard triggered by the worst case scenario in South China Sea, while the Manila Trench is becoming the most tsunami-hazardous subduction zone. In this study, the tsunami source of a new worst case scenario (Mw=9.3) is used for hazards assessment. The Okada model is taken to generate tsunami from Manila Trench based on the tsunami source parameters, while the shallow water equations are used to simulate the tsunami propagation from earthquake source to far-field region around South China Sea. The time series of surface elevation at measured locations near important cities along coasts and islands are investigated. The tsunami propagation scenarios, the arrival time, and tsunami wave distribution are obtained and analyzed for the assessment of tsunami hazard near coasts around South China Sea. Nested finer grid is used to simulate tsunami propagation to Hainan Island, Taiwan Island, and Lingding Bay for the worst case scenario. The regions with high level hazard are identified. ©© 2015 2015 The The Authors. Authors. Published Published by byElsevier Elsevier Ltd. Ltd This. is an open access article under the CC BY-NC-ND license (Peerhttp://creativecommons.org/licenses/by-nc-nd/4.0/-review under responsibility of The Chinese). -
Onland Signatures of the Palawan Microcontinental Block and Philippine Mobile Belt Collision and Crustal Growth Process: a Review
Journal of Asian Earth Sciences 34 (2009) 610–623 Contents lists available at ScienceDirect Journal of Asian Earth Sciences journal homepage: www.elsevier.com/locate/jaes Onland signatures of the Palawan microcontinental block and Philippine mobile belt collision and crustal growth process: A review Graciano P. Yumul Jr. a,b,*, Carla B. Dimalanta a, Edanjarlo J. Marquez c, Karlo L. Queaño d,e a National Institute of Geological Sciences, College of Science, University of the Philippines, Diliman, Quezon City, Philippines b Department of Science and Technology, Bicutan, Taguig City, Metro Manila, Philippines c Department of Physical Science and Mathematics, University of the Philippines-Manila, Philippines d School of Earth and Materials Science and Engineering, Mapua Institute of Technology, Intramuros, Manila, Philippines e Lands Geological Survey Division, Mines and Geosciences Bureau, Department of Environment and Natural Resources, North Avenue, Quezon City, Philippines article info abstract Article history: The collision of the Palawan microcontinental block with the Philippine mobile belt had significantly Received 14 April 2008 influenced the geological evolution of the Philippines. Multiple collisions involving several fragments, Received in revised form 7 October 2008 through space and time, resulted into the collage of terranes of varying origin exposed in this part of cen- Accepted 15 October 2008 tral Philippines. Cusping of the overriding plate, volcanic arc gap, ophiolite emplacement, incipient back- arc rifting, island rotation and tilting, raised coastal terraces, metamorphism, intrusion of igneous rocks and steepened subducted slab as seen in focal mechanism solutions are some of the manifestations of this Keywords: collision. A late Early Miocene to early Middle Miocene age (20–16 Ma) is proposed for the major collision Collision between the Palawan indenter and the Philippine mobile belt. -
Seabeam Survey at the Southern End of the Manila Trench
Tectonophjuics, 146 (1988) 261-278 261 Elsevier Science Publishers B.V., Amsterdam - Printed in The Netherlands Seabeam survey at the southern end of the Manila trench. ’ Transition between subduction and collision processes, I offshore Mindoro Island, Philippines i‘ li <I 1iig CLAUDE RANGIN JEAN FRANCOIS STEPHAN ’,RENE BLANCHET ’, DAVID BALADAD 3, PHILLIPE BOUYSEE 4, MIN PEN CHEN 5, PIERRE CHOTIN ’, JEAN YVES COLLOT 6, JACQUES DANIEL (’, JEAN MARCEL DROUHOT 7, YVES MARCHADIER BRUNQ MARSSET ’, BERNARD PELLETIER ‘, MARYANNICK RICHARD and MARC TARDY * ’ CNRS, UA 215 Département de Géotectonique, Université Pierre et Marie Curie, 4, Place Jussieu-Tour 26, 75252 Paris Cede-x O5 (France) ’CNRS, GIS, Océanologie et Géodvnaniie, Brest (France) ’BED, Manila (The Philippines) BRGM, Département de Géologie Marine, Orléuns (France) -‘National Taiwan Uniuersity (Taiwan) ‘Orstoni Centre de Noumea, Nouvelle Calédonie (New Caledonia) ’IFREMER Centre de Brest (France) Uniaersité de Savoie, Chambély (France) (Received May 11,1987; accepted May 28, 1987) Abstract Rangin, C., Stephan, J.F., Blanchet, R., Baladad, D., Bouysee, P., Chen, Min Pen, Chotin, P., Collot, J.Y., Daniel, J., Drouhot, J.M., Marchadier, Y., Marsset, B., Pelletier, B., Richard, M. and Tardy, M., 1988. Seabeam survey at the southern end of the Manila trench. Transition between subduction and collision processes, offshore Mindoro Island, Philippines. In: F.-C. Wezel (Editor), The Origin and Evolution of Arcs. Tectonopliysics, 146:261-278. The morphological and structural study conducted at the southern tip of the Manila trench, reveals that convergence between the South China Sea basin and Luzon is accommodated differently depending on the nature of the subducted slab. When the oceanic crust is subducted, a simple accretionary prism-fore arc basin pattern is developed.