Present-Day Crustal Motion in the Solomon Islands from GPS
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Playing Jigsaw with Large Igneous Provinces a Plate Tectonic
PUBLICATIONS Geochemistry, Geophysics, Geosystems RESEARCH ARTICLE Playing jigsaw with Large Igneous Provinces—A plate tectonic 10.1002/2015GC006036 reconstruction of Ontong Java Nui, West Pacific Key Points: Katharina Hochmuth1, Karsten Gohl1, and Gabriele Uenzelmann-Neben1 New plate kinematic reconstruction of the western Pacific during the 1Alfred-Wegener-Institut Helmholtz-Zentrum fur€ Polar- und Meeresforschung, Bremerhaven, Germany Cretaceous Detailed breakup scenario of the ‘‘Super’’-Large Igneous Province Abstract The three largest Large Igneous Provinces (LIP) of the western Pacific—Ontong Java, Manihiki, Ontong Java Nui Ontong Java Nui ‘‘Super’’-Large and Hikurangi Plateaus—were emplaced during the Cretaceous Normal Superchron and show strong simi- Igneous Province as result of larities in their geochemistry and petrology. The plate tectonic relationship between those LIPs, herein plume-ridge interaction referred to as Ontong Java Nui, is uncertain, but a joined emplacement was proposed by Taylor (2006). Since this hypothesis is still highly debated and struggles to explain features such as the strong differences Correspondence to: in crustal thickness between the different plateaus, we revisited the joined emplacement of Ontong Java K. Hochmuth, [email protected] Nui in light of new data from the Manihiki Plateau. By evaluating seismic refraction/wide-angle reflection data along with seismic reflection records of the margins of the proposed ‘‘Super’’-LIP, a detailed scenario Citation: for the emplacement and the initial phase of breakup has been developed. The LIP is a result of an interac- Hochmuth, K., K. Gohl, and tion of the arriving plume head with the Phoenix-Pacific spreading ridge in the Early Cretaceous. The G. -
Subsidence and Growth of Pacific Cretaceous Plateaus
ELSEVIER Earth and Planetary Science Letters 161 (1998) 85±100 Subsidence and growth of Paci®c Cretaceous plateaus Garrett Ito a,Ł, Peter D. Clift b a School of Ocean and Earth Science and Technology, POST 713, University of Hawaii at Manoa, Honolulu, HI 96822, USA b Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA Received 10 November 1997; revised version received 11 May 1998; accepted 4 June 1998 Abstract The Ontong Java, Manihiki, and Shatsky oceanic plateaus are among the Earth's largest igneous provinces and are commonly believed to have erupted rapidly during the surfacing of giant heads of initiating mantle plumes. We investigate this hypothesis by using sediment descriptions of Deep Sea Drilling Project (DSDP) and Ocean Drilling Program (ODP) drill cores to constrain plateau subsidence histories which re¯ect mantle thermal and crustal accretionary processes. We ®nd that total plateau subsidence is comparable to that expected of normal sea¯oor but less than predictions of thermal models of hotspot-affected lithosphere. If crustal emplacement was rapid, then uncertainties in paleo-water depths allow for the anomalous subsidence predicted for plumes with only moderate temperature anomalies and volumes, comparable to the sources of modern-day hotspots such as Hawaii and Iceland. Rapid emplacement over a plume head of high temperature and volume, however, is dif®cult to reconcile with the subsidence reconstructions. An alternative possibility that reconciles low subsidence over a high-temperature, high-volume plume source is a scenario in which plateau subsidence is the superposition of (1) subsidence due to the cooling of the plume source, and (2) uplift due to prolonged crustal growth in the form of magmatic underplating. -
Visualization of the Geophysical Settings in the Philippine Sea Margins by Means of GMT and ISC Data
Central European Journal of Geography and Sustainable Development 2020, Volume 2, Issue 1, Pages: 5-15 ISSN 2668-4322, ISSN-L 2668-4322 https://doi.org/10.47246/CEJGSD.2020.2.1.1 Visualization of the geophysical settings in the Philippine Sea margins by means of GMT and ISC data Polina Lemenkova* Ocean University of China, College of Marine Geo-sciences, 238 Songling Rd, Laoshan, 266100, Qingdao, Shandong, China; [email protected] Received: 22 February 2020; Revised: 12 March 2020; Accepted: 20 March 2020; Published online: 25 March 2020 _________________________________________________________________________________________________________________________ Abstract: The presented research aimed to perform geophysical modelling (gravity and geoid) and to evaluate the spatio-temporal variation of the marine geological data (distribution and depth of earthquakes) using combination of the Generic Mapping Tools (GMT) and available sources from the International Seismological Centre (ISC-EHB) that produce data on earthquakes as part of seismic survey and regional research projects. The target study area is a Philippine Sea basin (PSB) with two focused marginal areas: Philippine Trench and Mariana Trench, two hadal trenches located in the places of the tectonic plates subduction. Marine free-air gravity anomaly in the PSP shows higher values (>80 mGal) of the gravity fields structure at the volcanic areas and Philippine archipelago. Current study presented comparative geophysical analysis, and mapping free-air gravity and geoid in the Philippine Sea basin area. As a result of this study, the average level of earthquakes located in the Philippine Trench and Mariana Trench areas were compared, and those located in the Philippine archipelago are determined to be in the souther-western part (area of west Mindanao, south-west Visayas islands), while Luzon Islands shown shallower located earthquakes. -
Philippine Sea Plate Inception, Evolution, and Consumption with Special Emphasis on the Early Stages of Izu-Bonin-Mariana Subduction Lallemand
Progress in Earth and Planetary Science Philippine Sea Plate inception, evolution, and consumption with special emphasis on the early stages of Izu-Bonin-Mariana subduction Lallemand Lallemand Progress in Earth and Planetary Science (2016) 3:15 DOI 10.1186/s40645-016-0085-6 Lallemand Progress in Earth and Planetary Science (2016) 3:15 Progress in Earth and DOI 10.1186/s40645-016-0085-6 Planetary Science REVIEW Open Access Philippine Sea Plate inception, evolution, and consumption with special emphasis on the early stages of Izu-Bonin-Mariana subduction Serge Lallemand1,2 Abstract We compiled the most relevant data acquired throughout the Philippine Sea Plate (PSP) from the early expeditions to the most recent. We also analyzed the various explanatory models in light of this updated dataset. The following main conclusions are discussed in this study. (1) The Izanagi slab detachment beneath the East Asia margin around 60–55 Ma likely triggered the Oki-Daito plume occurrence, Mesozoic proto-PSP splitting, shortening and then failure across the paleo-transform boundary between the proto-PSP and the Pacific Plate, Izu-Bonin-Mariana subduction initiation and ultimately PSP inception. (2) The initial splitting phase of the composite proto-PSP under the plume influence at ∼54–48 Ma led to the formation of the long-lived West Philippine Basin and short-lived oceanic basins, part of whose crust has been ambiguously called “fore-arc basalts” (FABs). (3) Shortening across the paleo-transform boundary evolved into thrusting within the Pacific Plate at ∼52–50 Ma, allowing it to subduct beneath the newly formed PSP, which was composed of an alternance of thick Mesozoic terranes and thin oceanic lithosphere. -
Plate Tectonics and the Cycling of Earth Materials
Plate Tectonics and the cycling of Earth materials Plate tectonics drives the rock cycle: the movement of rocks (and the minerals that comprise them, and the chemical elements that comprise them) from one reservoir to another Arrows are pathways, or fluxes, the I,M.S rocks are processes that “reservoirs” - places move material from one reservoir where material is temporarily stored to another We need to be able to identify these three types of rocks. Why? They convey information about the geologic history of a region. What types of environments are characterized by the processes that produce igneous rocks? What types of environments are preserved by the accumulation of sediment? What types of environments are characterized by the tremendous heat and pressure that produces metamorphic rocks? How the rock cycle integrates into plate tectonics. In order to understand the concept that plate tectonics drives the rock cycle, we need to understand what the theory of plate tectonics says about how the earth works The major plates in today’s Earth (there have been different plates in the Earth’s past!) What is a “plate”? The “plate” of plate tectonics is short for “lithospheric plate” - - the outermost shell of the Earth that behaves as a rigid substance. What does it mean to behave as a rigid substance? The lithosphere is ~150 km thick. It consists of the crust + the uppermost mantle. Below the lithosphere the asthenosphere behaves as a ductile layer: one that flows when stressed It means that when the substance undergoes stress, it breaks (a non-rigid, or ductile, substance flows when stressed; for example, ice flows; what we call a glacier) Since the plates are rigid, brittle 150km thick slabs of the earth, there is a lot of “action”at the edges where they abut other plates We recognize 3 types of plate boundaries, or edges. -
Tectonic Setting & Generalized Geologic Maps of Washington And
on the Lea rs din e g ch E a . d e . g T e Tectonic Setting & Generalized Geologic Maps of Washington and Oregon The TO TLE Pict Earthquakes ure Frank D. Granshaw and Jenda Johnson, 2009 Volcanoes Tsunamis Geology1 Physical Geography Legend for Geography Relief map of Washington and Oregon showing Map colors correspond to vegetation Generalized geologic map of the Pacific Northwest. major cities, volcanoes, lakes and waterways. and surface types: (Circled numbers are the same as on Physical Geography legend) Greens—dense vegetation 1 Browns—grasslands and desert 1 A A Light gray to white—unvegetated alpine regions in the Cascade Range 2 2 Cities A Bellingham, WA N La Grande, OR B Seattle, WA O Baker, OR B I C Tacoma, WA P Ontario, OR B I D Olympia, WA B Bend, OR E Aberdeen, WA R Klamath Falls, OR C H C F Ellensberg, WA S Medford, OR E D 3 F G Yakima, WA T Coos Bay, OR D 3 H Wenatchee, WA U Newport, OR I Spokane, WA V Astoria ,OR G J Walla Walla, WA W Portland, OR G K Pasco, WA X Salem, OR K 4 4 5 L The Dalles, OR Y Eugene, OR 5 V V M Pendleton, OR J J Cascade Volcanoes M M L L W W 1 Mount Baker 6 Mount Hood 6 6 2 Glacier Peak 7 Mount Jeerson N N 3 Mount Rainier 8 Three Sisters 4 Mount St. Helens 9 Newberry Volcano X X 5 Mount Adams 10 Crater Lake O 7 7 Legend for Geology U U Igneous Rock 8 8 Q Q Y Y P Volcanic (Less than 1.6 million years) Volcanic (More than 1.6 million years) 9 9 Volcanic (Mostly 16.5- to 6-million- year-old flood basalts) T T Intrusive rock 10 Sedimentary and Metamorphic Rock 10 Unconsolidated sediment Sedimentary rock S Sedimentary & metamorphic rock R S R Metamorphic rock Physiographic Provinces2 Tectonics3 Map of major physiographic provinces in the Pacic Northwest. -
Presentation on Pacific Plate and Associated Boundaries
PACIFIC PLATE AND ASSOCIATED BOUNDARIES The Pacific Plate • Pacific Plate is the largest plate and an oceanic plate. • It shares its boundaries with numerous plates namely; North American Plate.(Convergent and transform fault) Philippine Plate.(Convergent) Juan de Fuca Plate.(Convergent) Indo – Australian Plate.(Convergent, Transform Fault) Cocos Plate.(Divergent) Nazca Plate.(Divergent) Antarctic Plate.(Divergent,Transform Fault) Types of Plate Boundaries • Convergent Boundary: Subduction zones where two plates converges. Eg; Aleutian Islands(Alaska) • Divergent Boundary: Spreading centres where two plates move away from each other. Eg; East Pacific Rise (MOR, Pacific Ocean). • Transform Faults: Boundary where two plates slide past each other. For Eg. ; San Andreas Fault. BOUNDARY WITH ANTARCTIC PLATE DIVERGENT BOUNDARY • Pacific – Antarctic Ridge TRANSFORM FAULT • Louisville Seamount Chain Pacific – Antarctic Ridge Pacific – Antarctic Ridge(PAR) is located on the seafloor of the South Pacific Ocean. It is driven by the interaction of a mid oceanic ridge and deep mantle plumes located in the eastern portion of East Pacific Ridge. Louisville Seamount Chain It is the longest line of seamount chain in the Pacific Ocean of about 4,300 km, formed along the transform boundary in the western side between Pacific plate and Antarctic plate. It was formed from the Pacific Plate sliding over a long – lived centre of upwelling magma called the Louisville hotspot. BOUNDARY WITH PHILIPPINE PLATE CONVERGENT BOUNDARY • Izu – Ogasawara Trench • Mariana Trench Izu – Ogasawara Trench It is an oceanic trench in the western Pacific Ocean. It stretches from Japan to northern most section of Mariana Trench. Here, the Pacific Plate is being subducted beneath the Philippine Sea Plate. -
Subduction History in the Melanesian Borderlands Region, SW Pacific
Subduction history in the Melanesian Borderlands region, SW Pacific Maria Seton1, Nicolas Flament, R. Dietmar Müller Keywords: Coral Sea, Melanesia, subduction, seafloor-spreading, SW Pacific, tectonics, geodynamics Abstract The easternmost Coral Sea region is an underexplored area at the northeasternmost corner of the Australian plate. Situated between the Mellish Rise, southern Solomon Islands, northern Vanuatu and New Caledonia, it represents one of the most dynamic and tectonically complex submarine regions of the world. Interactions between the Pacific and Australian plate boundaries have resulted in an intricate assemblage of deep oceanic basins and ridges, continental fragments and volcanic products; yet there is currently no clear conceptual framework to describe their formation. Due to the paucity of geological and geophysical data from the area to constrain plate tectonic models, a novel approach has been developed whereby the history of subduction based on a plate kinematic model is mapped to present-day seismic tomography models. A plate kinematic model, which includes a self-consistent mosaic of evolving plate boundaries through time is used to compute plate velocity fields and palaeo- oceanic age grids for each plate in 1 million year intervals. Figure 1. Regional digital elevation model (ETOPO2) of the eastern Coral Forward geodynamic models, with imposed surface plate velocity Sea. CT = Cato Trough, ERIR = East Rennell Island Ridge, LT = Louisiade trough, RFZ = Rennell Fracture Zone, RIR = Rennell Island Ridge, RT = constraints are computed using the 3D spherical finite element Rennell trough, SCT = San Cristobal Trench, SRT = South Rennell Trough, convection code CitcomS. A comparison between the present-day WTP = West Torres Plateau. -
Investigation 2: How Do We Recognize Plate Boundaries? Assessment
Investigation 2: How do we recognize plate boundaries? Assessment Answer the questions below in complete sentences. 1. What major plate lies west of the North American plate? The major plate west of the North American plate is the Pacific plate. 2. What plate lies northeast of the North American plate? The plate NE of the North American plate is the Eurasian plate. 3. What plate borders the North American plate to the southeast? The plate that borders the North American plate to the southeast is the African plate. 4. Which three plates border the North American plate to the south? The Caribbean, Cocos, and South American plates border the North American plate to the south. 5. What plate borders the North American plate in the U.S. Pacific Northwest? The plate that borders the North American plate in the U.S. Pacific Northwest is the Juan de Fuca Plate. 6. How are earthquakes and volcanoes related to plate boundaries? Earthquake clusters occur on or very near plate boundaries. Volcanoes occur about 100 kilometers away from a plate boundary in the overriding plate. 7. What kind of plate boundary separates the North American and Eurasian plates? A divergent plate boundary separates the North American and Eurasian plates. Copyright © 2012 Environmental Literacy and Inquiry Working Group at Lehigh University Investigation 2: Assessment 2 8. What kind of plate boundary separates the North American and Pacific plates at 31˚ latitude, -115˚ longitude? A transform plate boundary separates the North American and Pacific plates at 31˚ latitude, -115˚ longitude. 9. What kind of plate boundary separates the North American and Pacific plates at 55˚ latitude, -160˚ longitude? A convergent plate boundary separates the North American and Pacific plates at 55˚ latitude, -160˚ longitude. -
Intra-Panthalassa Ocean Subduction Zones Revealed by Fossil Arcs and Mantle Structure D
LETTERS PUBLISHED ONLINE: 26 FEBRUARY 2012 | DOI: 10.1038/NGEO1401 Intra-Panthalassa Ocean subduction zones revealed by fossil arcs and mantle structure D. G. van der Meer1,2*, T. H. Torsvik3,4,5,6, W. Spakman1*, D. J. J. van Hinsbergen3,6 and M. L. Amaru1,7 The vast Panthalassa Ocean once surrounded the supercon- unconstrained in the early Mesozoic Panthalassa Ocean4,11,12. tinent Pangaea. Subduction has since consumed most of the Notably, some of these terranes preserve relics of fossil Triassic and oceanic plates that formed the ocean floor, so classic plate Jurassic volcanic arc complexes that accreted many tens of millions reconstructions based on magnetic anomalies can be used of years after their extinction to circum-Pacific continents4,11,13. only to constrain the ocean’s history since the Cretaceous This shows that Triassic and Jurassic subduction zones existed away period1,2, and the Triassic–Jurassic plate tectonic evolution from continental margins in the Panthalassa Ocean. As subducted of the Panthalassa Ocean remains largely unresolved3,4. Ge- slab remnants (that is, subducted oceanic crust and lithosphere) ological clues come from extinct intra-oceanic volcanic arcs associated with these subduction zones might still reside in that formed above ancient subduction zones, but have since the lower mantle, the structure of the sub-Pacific mantle may been accreted to the North American and Asian continental provide palaeolongitudes of intra-oceanic subduction, allowing margins4. Here we compile data on the composition, the timing significant improvement of plate tectonic reconstructions of the of formation and accretion, and the present-day locations of early Mesozoic Panthalassa Ocean. -
What's the Difference?
New Zealand American Submarine Ring of Fire 2007 What’s The Difference? FOCUS SEATING ARRANGEMENT Volcanic processes at convergent and divergent Classroom style if students are working individu- tectonic plate boundaries ally, or groups of two to four students GRADE LEVEL MAXIMUM NUMBER OF STUDENTS 9-12 (Earth Science) 30 FOCUS QUESTION KEY WORDS How do volcanic processes differ at convergent Volcano and divergent tectonic plate boundaries? Caldera Hot spot LEARNING OBJECTIVES Ring of Fire Students will be able to compare and contrast Asthenosphere volcanoes at convergent and divergent plate Lithosphere boundaries. Magma Fault Students will be able to identify three geologic Transform boundary features that are associated with most volcanoes Convergent boundary on Earth. Divergent boundary Subduction Students will be able to explain why some volca- Tectonic plate noes erupt explosively while others do not. BACKGROUND INFORMATION MATERIALS The Submarine Ring of Fire is an arc of active vol- Copies of “Submarine Volcanism Worksheet,” canoes that partially encircles the Pacific Ocean one copy for each student or student group Basin, including the Kermadec and Mariana Islands in the western Pacific, the Aleutian Islands AUDIO/VISUAL MATERIALS between the Pacific and Bering Sea, the Cascade (Optional) Computer projection equipment to Mountains in western North America, and numer- show downloaded video materials ous volcanoes on the western coasts of Central America and South America. These volcanoes TEACHING TIME result from the motion of -
Post 8Ma Reconstruction of Papua New Guinea and Solomon Islands
ÔØ ÅÒÙ×Ö ÔØ Post 8 Ma reconstruction of Papua New Guinea and Solomon Islands: Microplate tectonics in a convergent plate boundary setting Robert J. Holm, Gideon Rosenbaum, Simon W. Richards PII: S0012-8252(16)30050-2 DOI: doi: 10.1016/j.earscirev.2016.03.005 Reference: EARTH 2238 To appear in: Earth Science Reviews Received date: 14 October 2015 Revised date: 14 January 2016 Accepted date: 11 March 2016 Please cite this article as: Holm, Robert J., Rosenbaum, Gideon, Richards, Simon W., Post 8 Ma reconstruction of Papua New Guinea and Solomon Islands: Microplate tectonics in a convergent plate boundary setting, Earth Science Reviews (2016), doi: 10.1016/j.earscirev.2016.03.005 This is a PDF file of an unedited manuscript that has been accepted for publication. As a service to our customers we are providing this early version of the manuscript. The manuscript will undergo copyediting, typesetting, and review of the resulting proof before it is published in its final form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. ACCEPTED MANUSCRIPT Post 8 Ma reconstruction of Papua New Guinea and Solomon Islands: Microplate tectonics in a convergent plate boundary setting Robert J. Holm 1, 2 , Gideon Rosenbaum 3, Simon W. Richards 1, 2 1Department of Earth and Oceans, College of Science, Technology & Engineering, James Cook University, Townsville, Queensland 4811, Australia 2Economic Geology Research Centre (EGRU), College of Science, Technology & Engineering, James Cook University, Townsville, Queensland 4811, Australia 3School of Earth Sciences, The University of Queensland, Brisbane, Queensland 4072, Australia corresponding author: [email protected] ABSTRACT Papua New Guinea and the Solomon Islands are located in a complex tectonic setting between the convergingACCEPTED Ontong Java Plateau MANUSCRIPT on the Pacific plate and the Australian continent.