From Oceanic Plateaus to Allochthonous Terranes: Numerical Modelling
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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. -
Geologic History of Siletzia, a Large Igneous Province in the Oregon And
Geologic history of Siletzia, a large igneous province in the Oregon and Washington Coast Range: Correlation to the geomagnetic polarity time scale and implications for a long-lived Yellowstone hotspot Wells, R., Bukry, D., Friedman, R., Pyle, D., Duncan, R., Haeussler, P., & Wooden, J. (2014). Geologic history of Siletzia, a large igneous province in the Oregon and Washington Coast Range: Correlation to the geomagnetic polarity time scale and implications for a long-lived Yellowstone hotspot. Geosphere, 10 (4), 692-719. doi:10.1130/GES01018.1 10.1130/GES01018.1 Geological Society of America Version of Record http://cdss.library.oregonstate.edu/sa-termsofuse Downloaded from geosphere.gsapubs.org on September 10, 2014 Geologic history of Siletzia, a large igneous province in the Oregon and Washington Coast Range: Correlation to the geomagnetic polarity time scale and implications for a long-lived Yellowstone hotspot Ray Wells1, David Bukry1, Richard Friedman2, Doug Pyle3, Robert Duncan4, Peter Haeussler5, and Joe Wooden6 1U.S. Geological Survey, 345 Middlefi eld Road, Menlo Park, California 94025-3561, USA 2Pacifi c Centre for Isotopic and Geochemical Research, Department of Earth, Ocean and Atmospheric Sciences, 6339 Stores Road, University of British Columbia, Vancouver, BC V6T 1Z4, Canada 3Department of Geology and Geophysics, University of Hawaii at Manoa, 1680 East West Road, Honolulu, Hawaii 96822, USA 4College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, 104 CEOAS Administration Building, Corvallis, Oregon 97331-5503, USA 5U.S. Geological Survey, 4210 University Drive, Anchorage, Alaska 99508-4626, USA 6School of Earth Sciences, Stanford University, 397 Panama Mall Mitchell Building 101, Stanford, California 94305-2210, USA ABSTRACT frames, the Yellowstone hotspot (YHS) is on southern Vancouver Island (Canada) to Rose- or near an inferred northeast-striking Kula- burg, Oregon (Fig. -
3.16 Oceanic Plateaus A.C.Kerr Cardiffuniversity,Wales,UK
3.16 Oceanic Plateaus A.C.Kerr CardiffUniversity,Wales,UK 3.16.1 INTRODUCTION 537 3.16.2 FORMATION OF OCEANIC PLATEAUS 539 3.16.3 PRESERVATIONOFOCEANIC PLATEAUS 540 3.16.4GEOCHEMISTRY OF CRETACEOUSOCEANICPLATEAUS 540 3.16.4.1 GeneralChemicalCharacteristics 540 3.16.4.2 MantlePlumeSource Regions ofOceanic Plateaus 541 3.16.4.3 Caribbean–ColombianOceanic Plateau(, 90 Ma) 544 3.16.4.4OntongJavaPlateau(, 122 and , 90 Ma) 548 3.16.5THE INFLUENCE OF CONTINENTALCRUST ON OCEANIC PLATEAUS 549 3.16.5.1 The NorthAtlantic Igneous Province ( , 60 Ma to Present Day) 549 3.16.5.2 The KerguelenIgneous Province ( , 133 Ma to Present Day) 550 3.16.6 IDENTIFICATION OF OCEANIC PLATEAUS IN THE GEOLOGICAL RECORD 551 3.16.6.1 Diagnostic FeaturesofOceanic Plateaus 552 3.16.6.2 Mafic Triassic Accreted Terranesinthe NorthAmericanCordillera 553 3.16.6.3 Carboniferous to CretaceousAccreted Oceanic Plateaus inJapan 554 3.16.7 PRECAMBRIAN OCEANICPLATEAUS 556 3.16.8ENVIRONMENTAL IMPACT OF OCEANICPLATEAU FORMATION557 3.16.8.1 Cenomanian–TuronianBoundary (CTB)Extinction Event 558 3.16.8.2 LinksbetweenCTB Oceanic PlateauVolcanism andEnvironmentalPerturbation 558 3.16.9 CONCLUDING STATEMENTS 560 REFERENCES 561 3.16.1 INTRODUCTION knowledge ofthe oceanbasins hasimproved over the last 25years,many moreoceanic plateaus Although the existence oflarge continentalflood havebeenidentified (Figure1).Coffinand basalt provinceshasbeenknownfor some Eldholm (1992) introduced the term “large igneous considerabletime, e.g.,Holmes(1918),the provinces” (LIPs) asageneric term encompassing recognition thatsimilarfloodbasalt provinces oceanic plateaus,continentalfloodbasalt alsoexist belowthe oceans isrelatively recent. In provinces,andthoseprovinceswhich form at the early 1970s increasingamounts ofevidence the continent–oceanboundary (volcanic rifted fromseismic reflection andrefraction studies margins). -
S41598-020-76691-1 1 Vol.:(0123456789)
www.nature.com/scientificreports OPEN Rifting of the oceanic Azores Plateau with episodic volcanic activity B. Storch1*, K. M. Haase1, R. H. W. Romer1, C. Beier1,2 & A. A. P. Koppers3 Extension of the Azores Plateau along the Terceira Rift exposes a lava sequence on the steep northern fank of the Hirondelle Basin. Unlike typical tholeiitic basalts of oceanic plateaus, the 1.2 km vertical submarine stratigraphic profle reveals two successive compositionally distinct basanitic to alkali basaltic eruptive units. The lower unit is volumetrically more extensive with ~ 1060 m of the crustal profle forming between ~ 2.02 and ~ 1.66 Ma, followed by a second unit erupting the uppermost ~ 30 m of lavas in ~ 100 kyrs. The age of ~ 1.56 Ma of the youngest in-situ sample at the top of the profle implies that the 35 km-wide Hirondelle Basin opened after this time along normal faults. This rifting phase was followed by alkaline volcanism at D. João de Castro seamount in the basin center indicating episodic volcanic activity along the Terceira Rift. The mantle source compositions of the two lava units change towards less radiogenic Nd, Hf, and Pb isotope ratios. A change to less SiO2-undersaturated magmas may indicate increasing degrees of partial melting beneath D. João de Castro seamount, possibly caused by lithospheric thinning within the past 1.5 million years. Our results suggest that rifting of oceanic lithosphere alternates between magmatically and tectonically dominated phases. Oceanic plateaus with a crustal thickness to 30 km cover large areas in the oceans and these bathymetric swells afect oceanic currents and marine life 1,2. -
Active Continental Margin
Encyclopedia of Marine Geosciences DOI 10.1007/978-94-007-6644-0_102-2 # Springer Science+Business Media Dordrecht 2014 Active Continental Margin Serge Lallemand* Géosciences Montpellier, University of Montpellier, Montpellier, France Synonyms Convergent boundary; Convergent margin; Destructive margin; Ocean-continent subduction; Oceanic subduction zone; Subduction zone Definition An active continental margin refers to the submerged edge of a continent overriding an oceanic lithosphere at a convergent plate boundary by opposition with a passive continental margin which is the remaining scar at the edge of a continent following continental break-up. The term “active” stresses the importance of the tectonic activity (seismicity, volcanism, mountain building) associated with plate convergence along that boundary. Today, people typically refer to a “subduction zone” rather than an “active margin.” Generalities Active continental margins, i.e., when an oceanic plate subducts beneath a continent, represent about two-thirds of the modern convergent margins. Their cumulated length has been estimated to 45,000 km (Lallemand et al., 2005). Most of them are located in the circum-Pacific (Japan, Kurils, Aleutians, and North, Middle, and South America), Southeast Asia (Ryukyus, Philippines, New Guinea), Indian Ocean (Java, Sumatra, Andaman, Makran), Mediterranean region (Aegea, Cala- bria), or Antilles. They are generally “active” over tens (Tonga, Mariana) or hundreds (Japan, South America) of millions of years. This longevity has consequences on their internal structure, especially in terms of continental growth by tectonic accretion of oceanic terranes, or by arc magmatism, but also sometimes in terms of continental consumption by tectonic erosion. Morphology A continental margin generally extends from the coast down to the abyssal plain (see Fig. -
The Saharides and Continental Growth During the Final Assembly of Gondwana-Land
Reconstructing orogens without biostratigraphy: The Saharides and continental growth during the final assembly of Gondwana-Land A. M. Celâl S¸ engöra,b,1, Nalan Lomc, Cengiz Zabcıb, Gürsel Sunalb, and Tayfun Önerd aIstanbul_ Teknik Üniversitesi (ITÜ)_ Avrasya Yerbilimleri Enstitüsü, Ayazaga˘ 34469 Istanbul,_ Turkey; bITÜ_ Maden Fakültesi, Jeoloji Bölümü, Ayazaga˘ 34469 Istanbul,_ Turkey; cDepartement Aardwetenschappen, Universiteit Utrecht, 3584 CB Utrecht, The Netherlands; and dSoyak Göztepe Sitesi, Üsküdar 34700 Istanbul,_ Turkey Contributed by A. M. Celâl S¸ engör, October 3, 2020 (sent for review July 17, 2020; reviewed by Jonas Kley and Leigh H. Royden) A hitherto unknown Neoproterozoic orogenic system, the Sahar- identical to those now operating (the snowball earth and the ab- ides, is described in North Africa. It formed during the 900–500-Ma sence of land flora were the main deviating factors), yet the interval. The Saharides involved large subduction accretion com- dominantly biostratigraphy-based methods used to untangle oro- plexes occupying almost the entire Arabian Shield and much of genic evolution during the Phanerozoic are not applicable Egypt and parts of the small Precambrian inliers in the Sahara in- to them. cluding the Ahaggar mountains. These complexes consist of, at least by half, juvenile material forming some 5 million km2 new Method of Reconstructing Complex Orogenic Evolution in continental crust. Contrary to conventional wisdom in the areas the Neoproterozoic without Biostratigraphy: Example of the they occupy, -
Bering Sea in Summer of 1955
OCEANOGRAPHIC CONDITIONS OF THE WHALING GROUNDS IN THE WATERS ADJACENT TO ALEUTIAN ISLANDS AND THE BERING SEA IN SUMMER OF 1955 KEIJI NASU INTRODUCTION The present paper gives the outline of the results investigated by Japa nese research members in the waters adjacent to Aleutian Islands and the Bering Sea during the Whaling Survey including whale-marking ex periment in the summer of 1955 on boad of the "Konan-maru No. 5 ", be longing to the Nippon Suisan Co. Ltd. During the season, 73 Stations were occupied by the boat as shown in figure 1, the observed data at these stations are compiled with respect to the oceanographic elements such as water temperature, salinity (chlorinity), transparency of the sea water, colour of the sea water, dissolved oxygen, planktons, and other sea living organisms sampled from various depths, and also with the weather elements such as air temperature, sea-fog etc. Above materials are collected on board by the author and Takehiko Kawakami of the Japa nese Fisheries Agency. The author wishes to express his hearty thanks to Dr. Michitaka Uda, Professor of the Tokyo University of Fisheries and also to Mr. Makoto Ishino for their instructions and aids given during the preparation of this report. WATER TEMPERATURE AND SALINITY AT THE SEA SURF ACE The surface temperature in the period during the survey from early July to late September in the Bering Sea and the southern Aleutian Waters in the North Pacific vary from 11.8°C at its maximum to the lowest value 6.5°C. In general the isothermal lines run parallel to the Aleutian Islands from west to east. -
The Shatsky Rise Oceanic Plateau Structure from Two-Dimensional Multichannel Seismic Refl Ection Profi Les and Implications for Oceanic Plateau Formation
Downloaded from specialpapers.gsapubs.org on June 2, 2015 The Geological Society of America Special Paper 511 2015 The Shatsky Rise oceanic plateau structure from two-dimensional multichannel seismic refl ection profi les and implications for oceanic plateau formation Jinchang Zhang* William W. Sager† Department of Oceanography, Texas A&M University, College Station, Texas 77843, USA Jun Korenaga Department of Geology and Geophysics, Yale University, New Haven, Connecticut 06520, USA ABSTRACT The Shatsky Rise is one of the largest oceanic plateaus, a class of volcanic fea- tures whose formation is poorly understood. It is also a plateau that was formed near spreading ridges, but the connection between the two features is unclear. The geologic structure of the Shatsky Rise can help us understand its formation. Deeply penetrating two-dimensional (2-D) multichannel seismic (MCS) refl ection profi les were acquired over the southern half of the Shatsky Rise, and these data allow us to image its upper crustal structure with unprecedented detail. Synthetic seismo- grams constructed from core and log data from scientifi c drilling sites crossed by the MCS lines establish the seismic response to the geology. High-amplitude basement refl ections result from the transition between sediment and underlying igneous rock. Intrabasement refl ections are caused by alternations of lava fl ow packages with dif- fering properties and by thick interfl ow sediment layers. MCS profi les show that two of the volcanic massifs within the Shatsky Rise are immense central volcanoes. The Tamu Massif, the largest (~450 km × 650 km) and oldest (ca. 145 Ma) volcano, is a single central volcano with a rounded shape and shallow fl ank slopes (<0.5°–1.5°), characterized by lava fl ows emanating from the volcano center and extending hun- dreds of kilometers down smooth, shallow fl anks to the surrounding seafl oor. -
Oceanic Plateau and Island Arcs of Southwestern Ecuador: Their Place in the Geodynamic Evolution of Northwestern South America
Reprinted from TECTONOPHYSICS INTERNATIONAL JOURNAL OF GEOTECTONICS AND THE GEOLOGY AND PHYSICS OF THE INTERIOR OF THE EARTH Tectonophysics 307 (1999) 235-254 Oceanic plateau and island arcs of southwestern Ecuador: their place in the geodynamic evolution of northwestern South America Cédric Reynaud a, fitienne Jaillard a,b, Henriette Lapierre al*, Marc Mamberti %c, Georges H. Mascle a '' UFRES, A-5025, Université Joseph Fourier; Institut Doloniieu, 15 rue Maurice-Gignoux, 38031 Grenoble cedex, Francel IO, "IRD lfoniierly ORSTOM), CSI, 209-213 rue Lu Fayette, 75480 Faris cedex France 'Institut de Minéralogie et Fétrogrphie, Université de Lausanne, BFSH2 (3171), I015 Lausanne, Switzerland Received 12 August 1997; accepted 11 March 1999 Fonds Documentaire ORSTOM 9" ELSEVIER Cote :&e4 973 9 Ex : LII>f c.- TECTONOPHYSICS Editors-in-Chief J.-P. BURG ETH-Zentrum, Geologisches Institut, Sonneggstmße 5, CH-8092, Zürich, Switzerland. Phone: +41.1.632 6027; FAX: +41.1.632 1080; e-mail: [email protected] T. ENGELDER Pennsylvania State University, College of Earth & Mineral Sciences, 336 beike Building, University Park, PA 16802, USA. Phone: +I .814.865.3620/466.7208; FAX: +I .814.863.7823; e-mail: engelderOgeosc.psu.edu K.P. FURLONG Pennsylvania State University, Department of Geosciences, 439 Deike Building, University Park, PA 16802, USA. Phone: +1 .814.863.0567; FAX: +1.814.865.3191; e-mail: kevinOgeodyn.psu.edu F. WENZEL Universität Fridericiana Karlsruhe, Geophysikalisches Institut, Hertzstraße Bau Karlsruhe, Germany. .physik.uni-karlsruhe.de16, 42, D-76187 Phone: +49.721.608 4431; FAX +49.721.711173; e-mail: fwenzel@gpiwapl Honorary Editor: S. Uyeda Editorial Board Z. -
Habitat and Environment of Islands— Primary and Supplemental Island Sets
Habitat and Environment of Islands— Primary and Supplemental Island Sets Professional Paper 1590 EXPLANATION Primary Island Set Supplemental Island Set A Supplemental Island Set B U.S. Department of the Interior U.S. Geological Survey HABITAT AND ENVIRONMENT OF ISLANDS Primary and Supplemental Island Sets By N.C. Matalas and Bernardo F. Grossling U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1590 U.S. Department of the Interior GALE A. NORTON, Secretary U.S. GEOLOGICAL SURVEY Charles G. Groat, Director Any use of trade, product, or firm names in this report is for identification purposes only and does not constitute endorsement by the U.S. Government Reston, Virginia 2002 Library of Congress Cataloging-in-Publication Data Matalas, Nicholas C., 1930– Habitat and environment of islands : primary and supplemental island sets / by N.C. Matalas and Bernardo F. Grossling. p. cm. — (U.S. Geological Survey professional paper ; 1590) Includes bibliographical references (p. ). ISBN 0-607-99508-4 1. Island ecology. 2. Habitat (Ecology) I. Grossling, Bernardo F., 1918– II. Title. III. Series. QH541.5.I8 M27 2002 577.5’2—dc21 2002035440 For sale by the U.S. Geological Survey Information Services Box 25286, Federal Center, Denver, CO 80225 PREFACE The original intent of the study was to develop a first-order synopsis of island hydrology with an inte- grated geologic basis on a global scale. As the study progressed, the aim was broadened to provide a frame- work for subsequent assessments on large regional or global scales of island resources and impacts on -
Future Accreted Terranes: a Compilation of Island Arcs, Oceanic Plateaus, Submarine Ridges, Seamounts, and Continental Fragments” by J
Open Access Solid Earth Discuss., 6, C1212–C1222, 2014 www.solid-earth-discuss.net/6/C1212/2014/ Solid Earth © Author(s) 2014. This work is distributed under Discussions the Creative Commons Attribute 3.0 License. Interactive comment on “Future accreted terranes: a compilation of island arcs, oceanic plateaus, submarine ridges, seamounts, and continental fragments” by J. L. Tetreault and S. J. H. Buiter J. L. Tetreault and S. J. H. Buiter [email protected] Received and published: 30 October 2014 Response to Review C472: M. Pubellier I thank M. Pubellier for his in-depth review; the suggestions are very constructive and have truly improved the manuscript. I will first reply to the review letter below, and then to points in the supplement that need further explanation/discussion. Otherwise, if the point is not addressed, it has simply been corrected. In the review letter, the reviewer writes: I agree with most of the results presented in this paper but I regret a bit that the empha- C1212 sis was a bit too much on ancient examples (except the Solomon Islands and Taiwan that has been just mentioned). The authors could give more attention to the recent examples such as Southeast Asia. I have suggested some examples (which of course are those I know well) for reference; but there are others. I am sorry to have put some references of papers for which I participated but it is just for the sake of discussion. I think some examples of recent tectonics bring elements in this interesting discussion. The reviewer comments that my paper is quite heavy on ancient examples of accreted terranes, and I admit, now looking back on my review, that it was done so, albeit sub- consciously. -
Submarine Plateau Volcanism and Cretaceous Ocean Anoxic Event 1A: Geochemical Evidence from Aptian Sedimentary Sections
AN ABSTRACT OF THE THESIS OF Paul Steven Walczak for the degree of Master of Science in Oceanography presented on May 30, 2006. Title: Submarine Plateau Volcanism and Cretaceous Ocean Anoxic Event 1a: Geochemical Evidence from Aptian Sedimentary Sections. Abstract approved: _____________________________________________________________________ Robert A. Duncan Marine sediments exceptionally rich in organic carbon, known as black shales, occur globally but intermittently in well correlated Cretaceous successions. The presence of black shales indicates that sporadic, ocean-wide interruption of normal respiration of marine organic matter during oxygen-deficient conditions has occurred. Submarine volcanism on a massive scale, related to the construction of ocean plateaus, could be responsible for the abrupt onset and conclusion of these Ocean Anoxic Events (OAEs), via the oxidation of magmatic effluent, the stimulation of increased primary productivity, and the resultant respiration of sinking organic matter. These discrete periods of global ocean anoxia are accompanied by trace metal enrichments that are coincident with magmatic activity and hydrothermal exchange during plateau construction. The link between submarine volcanism associated with the emplacement of the Ontong Java - Manihiki plateau (~122 Ma) and Cretaceous Ocean Anoxic Event 1a is explored in this study. Two marine sedimentary sections, recovered in cores from Deep Sea Drilling Program (DSDP) Site 167 (Magellan Rise) and Site 463 (Mid-Pacific Mountains), were analyzed for a suite of major, minor, and trace elements. Trace element abundance patterns for these locations were compared to similar data from the CISMON core (Belluno Basin, Northern Italy) to determine if a relationship existed between the timing of trace metal anomalies and global biogeochemical events.