432 Iapetus Ocean Iapetus Ocean Atlantic Ocean N, Precambrian
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Ontong Java and Kerguelen Plateaux: Cretaceous Icelands?
Journal of the Geological Society, London, Vol. 152, 1995, pp. 1047-1052, 4 figs. Printed in Northern Ireland Ontong Java and Kerguelen Plateaux: Cretaceous Icelands? M. F. COFFIN & L.M. GAHAGAN Institute for Geophysics, The University of Texas at Austin, 8701 North Mopac Expressway, Austin, Texas 78759-8397, USA Abstract: Together with Iceland, the two giant oceanic plateaux, Ontong Java in the western Pacific and Kerguelen/Broken Ridge in the Indian Ocean, are accumulations of mafic igneous rock which were not formed by 'normal' seafloor spreading. We compare published geochronological, crustal structure, and subsidence results with tectonic fabric highlighted in new satellite-derived free-air gravity data from the three igneous provinces, and conclude that existing evidence weighs lightly against the Ontong Java and Kerguelen plateaux originating at a seafloor spreading centre. Keywords: Iceland, Ontong Java Plateau, Kerguelen Plateau, plumes, hot spots. The two giant oceanic plateaux, Ontong Java in the western Age constraints Pacific, and Kerguelen in the south-central Indian Ocean (Fig. 1), and Iceland are among the best-studied examples of The vast bulk of crust in the ocean basins is dated using large-scale mafic magmatism not resulting solely from magnetic anomalies created by the interplay between the 'normal' seafloor spreading. Analogues on the continents, seafloor spreading process and the alternating polarity of the continental flood basalts, are demonstrably not created by Earth's magnetic field. Mesozoic and Cenozoic marine seafloor spreading, although controversy persists as to magnetic anomalies, summarized globally by Cande et al. whether or not lithospheric extension must precede their (1989), are most commonly tied to geological time through emplacement. -
Volume 144 Index
Index to Volume 144 INDEX TO VOLUME 144 This index provides coverage for both the Initial Reports and Scientific Results portions of Volume 144 of the Proceedings of the Ocean Drilling Program. Refer- ences to page numbers in the Initial Reports are preceded by “A” with a colon (A:), and to those in the Scientific Results (this book), by “B” with a colon (B:). In addi- tion, reference to material on CD-ROM is shown as “bp:CD-ROM.” The index was prepared by Earth Systems, under subcontract to the Ocean Drill- ing Program. The index contains two hierarchies of entries: (1) a main entry, defined as a keyword or concept followed by a reference to the page on which that word or concept appears, and (2) a subentry, defined as an elaboration on the main entry fol- lowed by a page reference. The index is presented in two parts: (1) a Subject Index and (2) a Taxonomic Index. Both parts cover text, figures, and tables but not core-description forms (“barrel sheets”), core photographs, smear-slide data, or thin-section descriptions; these are given in the Initial Reports. Also excluded from the index are biblio- graphic references, names of individuals, and routine front and back matter. The Subject Index follows a standard format. Geographic, geologic, and other terms are referenced only if they are subjects of discussion. This index also includes broad fossil groups such as nannofossils and radiolarians. A site chapter in the Ini- tial Reports is considered the principal reference for that site and is indicated on the first line of the site’s listing in the index. -
Modern and Ancient Hiatuses in the Pelagic Caps of Pacific Guyots and Seamounts and Internal Tides GEOSPHERE; V
Research Paper GEOSPHERE Modern and ancient hiatuses in the pelagic caps of Pacific guyots and seamounts and internal tides GEOSPHERE; v. 11, no. 5 Neil C. Mitchell1, Harper L. Simmons2, and Caroline H. Lear3 1School of Earth, Atmospheric and Environmental Sciences, University of Manchester, Manchester M13 9PL, UK doi:10.1130/GES00999.1 2School of Fisheries and Ocean Sciences, University of Alaska-Fairbanks, 905 N. Koyukuk Drive, 129 O’Neill Building, Fairbanks, Alaska 99775, USA 3School of Earth and Ocean Sciences, Cardiff University, Main Building, Park Place, Cardiff CF10 3AT, UK 10 figures CORRESPONDENCE: neil .mitchell@ manchester ABSTRACT landmasses were different. Furthermore, the maximum current is commonly .ac .uk more important locally than the mean current for resuspension and transport Incidences of nondeposition or erosion at the modern seabed and hiatuses of particles and thus for influencing the sedimentary record. The amplitudes CITATION: Mitchell, N.C., Simmons, H.L., and Lear, C.H., 2015, Modern and ancient hiatuses in the within the pelagic caps of guyots and seamounts are evaluated along with of current oscillations should therefore be of interest to paleoceanography, al- pelagic caps of Pacific guyots and seamounts and paleotemperature and physiographic information to speculate on the charac- though they are not well known for the geological past. internal tides: Geosphere, v. 11, no. 5, p. 1590–1606, ter of late Cenozoic internal tidal waves in the upper Pacific Ocean. Drill-core Hiatuses in pelagic sediments of the deep abyssal ocean floor have been doi:10.1130/GES00999.1. and seismic reflection data are used to classify sediment at the drill sites as interpreted from sediment cores (Barron and Keller, 1982; Keller and Barron, having been accumulating or eroding or not being deposited in the recent 1983; Moore et al., 1978). -
Deep Sea Drilling Project Initial Reports Volume 20
31. BIOSTRATIGRAPHIC SYNTHESIS, LEG 20, DSDP Helen P. Foreman, Department of Geology, Oberlin College, Oberlin, Ohio Heinz Hekel, Geological Survey of Queensland, Brisbane, Australia Robert H. Hoskins, New Zealand Geological Survey, Lower Hutt, New Zealand and Valeri A. Krasheninnikov, Geological Institute of the Academy of Sciences of the USSR, Moscow, USSR INTRODUCTION Abundance and Preservation of Fossil Groups Figures 2 and 3 have been included to aid the reader in Setting selecting samples for further study. They indicate the Leg 20, which cruised.from Yokohama, Japan, to Suva, abundance and preservation of various fossil groups encoun- Fiji Islands, drilled 12 holes at eight sites as follows: tered. In requesting samples it should be kept in mind that Site 194: 33°58.66'N; 148°48.64'E Radiolaria in Cores 194-3, 1944, 194-5, 195-3, and 1954 Site 195: 32°46.5'N; 146°59.0'E were recovered only from cherts in the core catcher, in Site 196: 30°06.97'N; 148°34.49'E Core 195-5 from the center bit, and Core 195A-l from the Site 197: 30°17.44'N; 147°40.46'E bit; nannofossils in Cores 1954, 195-5, and 195A-1 were Site 198: 25°49.54'N; 154°35.05'E recovered only from the center bit. Site 199: 13°30.78'N; 156°10.34'E Site 200: 12°50.20'N; 156°46.96'E Site 201: 12°49.89'N; 156°44.59'E COMPARISON OF AGE AND ZONAL ASSIGNMENTS Site 202: 12°48.90'N; 156°57.15'E For Holes 194, 195, 195B, 196, and 198 it is not The location of Leg 20 sites in relation to bathymetry is possible to compare zones for the various faunal groups shown in Figure 1. -
Article (PDF, 2454
J.micropaZaeontol., 5 (1): 91-108, April 1986 A comparative study of collections from the S.W. Pacific (Saipan to Tonga), with the descriptions of GambieZZa caudata (Brady, 1890) and a new species of Pterobairdia (Ostracoda) K. G. McKENZlE Riverina-Murray Institute of Higher Education, Wagga Wagga, N.S.W., 2650, Australia ABSTRACT4ambielln caudata (Brady, 1890) and Pterobairdia briggsae sp. nov. are described from collections made in the S.W. Pacific (Saipan, Onotoa, Ontong-Java/Kula Gulf, Nournea, Cook Islands, Fiji, Samoa, Tonga); and the lectotypes of several species described in a major early paper by Brady (1890) are illustrated. The carbonate compensation depth in this region lies at around 4500m. Comparison of the Ontong-Java in Kula Gulf samples reinforces consideration of depth as a factor of ecological importance. A similarity matrix for the several faunas shows factors in common at species level ranging from 22% (0notoa:Noumea) to nearly 60% (Samoa/Onotoa); while endemism ranges from 8.5% (Samoa) to nearly 33% (Tonga). "ost endemic species belong in a limited number of podocopid families, in par- ticular Bairdiidae, Trachyleberididae, Paradoxostomatidae and Leptocytheridae. These results appear consistent with an hypothesis that continued tectonics-driven changes in the regional marine topography and sedimentation, i.e. niche development, could have triggered speciation along the regional plate margins. INTRODUCTION 1890 remains the major taxonomic reference) although A study of Ostracoda and other microfauna from the recently this undesirable situation has begun to improve S. W. Pacific commenced in 1980. It is based on material (Whatley, 1983). sampled during a number of cruises coordinated by CCOP/SOPAC (Committee for Coordination of Joint SAMPLE DESCRIPTIONS Prospecting for Mineral Resources in South Pacific Off- Preliminary sample descriptions of washings provided shore Areas). -
Thin Crust As Evidence for an Inherited Mantle Depletion Supporting the Marion Rise
Thin Crust as Evidence for an Inherited Mantle Depletion Supporting the Marion Rise Huaiyang Zhou* and Henry JB Dick** *State Key Laboratory of Marine Geology, Tongji University, Shanghai, China **Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA … …… …… …… …… …… …… …… …… …… …… …… …… …… …… ….. … The global ridge system is dominated by oceanic rises reflecting large variations in axial depth associated with mantle hotspots. The little studied Marion Rise is as large as the Icelandic, considering length and depth, but has an axial rift rather than a high nearly its entire length. Uniquely, along the SW Indian Ridge systematic sampling allows direct examination of crustal architecture over its full length. Unlike Iceland, peridotites are extensively exposed high over the rise. This shows for the 1st time that the crust is generally thin, and often missing over a rifted rise. Thus the rise must be largely an isostatic response to ancient melting events that created low-density depleted mantle beneath the ridge rather than thickened crust and/or a large thermal anomaly. The likely origin for the depleted mantle is that emplaced into the African asthenosphere during the Karoo and Madagascar flood basalt events. Following Morgan 1, common wisdom equates oceanic rises to a hot fertile mantle plume producing a flow of plume-derived mantle to the ridge and down the sub-axial asthenospheric channel, resulting in elevated mantle temperature, ridge topography, and thickened igneous crust (the mantle wedge hypothesis, e.g.: 2). Studies of the Reykjanes Ridge support this, with seismic crust thickening from ~6 km near the Gibbs FZ for 1600 km to ~18 km at the Reykjanes Peninsula e.g.: 3. -
Understanding the Physical Behavior of Volcanoes Steven N
Cambridge University Press 0521592542 - Volcanoes and the Environment Edited by Joan Marti and Gerald Ernst Excerpt More information Chapter 1 Understanding the physical behavior of volcanoes Steven N. Carey Introduction Each eruption represents a unique culmination of this complex series of steps, making the predic- Volcanism is a spectacular display of the com- tion of volcanic eruptions one of the most chal- plex way in which energy and materials are lenging tasks in the geosciences. exchanged between three major components of The science of volcanology draws from many our planet: the solid Earth, oceans, and atmo- different fields, including petrology, geochem- sphere. Mankind has long been both fascinated istry, seismology, and sedimentology. It began and terrified by erupting volcanoes. Yet through- with mainly qualitative observations about the out history people have been drawn to their fer- distribution of volcanoes, their eruptive behavior, tile slopes and have developed a unique sym- and the types of products they create. In AD 79, biosis. In many cultures, volcanoes symbolize a Pliny the Younger made the first written descrip- source of tremendous power that must be pla- tion of a volcanic eruption in two letters describ- cated by worship or sacrifice. Volcanologists, on ing the death of his uncle, Pliny the Elder, during the other hand, strive to understand how volca- the eruption of Vesuvius volcano in Italy. During noes work in order to better predict their behav- the past two decades the field of volcanology has iour and reduce the hazards to people who live undergone revolutionary changes in the under- near them. -
4. Upper Oligocene to Pleistocene Ostracoda from Guyots in the Western Pacific: Holes 871A, 872C, and 873B1
Haggerty, J.A., Premoli Silva, I., Rack, F., and McNutt, M.K. (Eds.), 1995 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 144 4. UPPER OLIGOCENE TO PLEISTOCENE OSTRACODA FROM GUYOTS IN THE WESTERN PACIFIC: HOLES 871A, 872C, AND 873B1 Robin Whatley2 and Ian Boomer2 ABSTRACT Assemblages of upper Oligocene to Pleistocene Ostracoda are described from pelagic sediments capping three guyots in the western Pacific Ocean. Recent studies have shown that a high percentage of seamount Ostracoda are restricted (i.e., endemic) to these bathymetrically isolated sites. In the following we detail changes in the Ostracoda (diversity, abundance, dominance, endemism, faunal turnover) from upper Oligocene to Pleistocene sediments encountered during Ocean Drilling Program Leg 144. Our results support previous observations on guyots and indicate that their high levels of endemism do not simply reflect a poor knowledge of the fauna in that region but truly reflect their bathymetrical isolation. Furthermore, whatever global event or events affected the deep-sea Ostracoda during the Miocene, the guyot faunas were not isolated from these changes. INTRODUCTION for the Pliocene-Pleistocene interval of a number of non-guyot, Pa- cific deep-sea sites range from 5% to 25%, compared with a range As our knowledge of deep-sea Ostracoda has advanced, it has from 50% to 60% for the Horizon (DSDP Sites 200/202) and Ita Mai become apparent that there exists in modern to Tertiary oceans both a Tai (DSDP Sites 44 and 171) guyots during the same interval. widespread pandemic element and regional, more endemic taxa The bathymetric isolation of the guyot summits has resulted in (Whatley and Ayress, 1988; Coles et al., 1990). -
40. Magmatic Development of the Southeast Greenland Margin and Evolution of the Iceland Plume: Geochemical Constraints from Leg 1521
Saunders, A.D., Larsen, H.C., and Wise, S.W., Jr. (Eds.), 1998 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 152 40. MAGMATIC DEVELOPMENT OF THE SOUTHEAST GREENLAND MARGIN AND EVOLUTION OF THE ICELAND PLUME: GEOCHEMICAL CONSTRAINTS FROM LEG 1521 Andrew D. Saunders,2 Hans Christian Larsen,3 and J. Godfrey Fitton4 ABSTRACT Leg 152, located on the southeast Greenland Margin, successfully recovered igneous rocks from three drill sites along a transect at 63°N: 915, 917, and 918. The margin is characterized by a 150-km-wide sequence of seaward-dipping reflectors (SDRS), and thus has an architecture typical of volcanic rifted margins. Site 917 was located close to the inboard, feather-edge of the SDRS, on the continental shelf, and drilling recovered rocks ranging in composition from picrite to dacite. Site 915 was immediately oceanward of Site 917, and Site 918 was located on the continental rise, in the main sequence of the SDRS. Drill- ing at both Sites 915 and 918 recovered basalt. Ash horizons were cored in the sediment column at Site 918 and Site 919 in the Irminger Basin. The oldest recovered lavas (the Lower and Middle Series from Site 917), erupted approximately 61 m.y. ago, sit on steeply dipping pre-rift metasediments. They are variably contaminated by ancient amphibolite- and granulite-facies crust, consistent with eruption in a continental setting before plate breakup. A few of the Lower Series lavas are high-MgO basalts. The amount of contamination decreased dramatically in the succeeding Upper Series lavas, which also show evidence for a rapid shallowing of the average depth of melting, and contain a high proportion of picrites and high-MgO basalts. -
Hotspots a Mantle Plume Under Iceland Is Taken for Granted As The
Hotspots Plumes, or plate tectonic processes? Abstract A mantle plume under Iceland is taken for granted as the cause of the Hotspots – large volcanic provinces – such volcanism there. But Gill Foulger argues that the evidence does not stand up. as Iceland, Hawaii and Yellowstone, are almost universally assumed to come from plumes of hot mantle rising from deep within the Earth. At Iceland, perhaps the best-studied hotspot on Earth, this hypothesis is inconsistent with many first- order observations, such as the lack of high temperatures, a volcanic track or a seismic anomaly in the lower mantle. The great melt production there is explained better by enhanced fertility in the mantle where the mid-Atlantic spreading ridge crosses the Caledonian suture zone. The thick crust built by the excessive melt production encourages complex, unstable, leaky microplate tectonics, which provides positive feedback by enhancing volcanism further. Such a model explains Iceland as a natural consequence of relatively shallow 1: Numerical simulation of a deep mantle plume. The red, mushroom-like feature represents a hot upwelling processes related to plate tectonics, and from the core–mantle boundary. Blue, linear features are cold downwellings. (From Kiefer and Kellogg 1998.) accounts for all the first- and second-order geophysical, geological and geochemical “hotspots”, i.e. areas of exceptionally intense scientists were afraid to question this radical observations at Iceland without special volcanism such as Hawaii, Yellowstone and new hypothesis because of their recent humili- pleading or invoking coincidences. Iceland, are fuelled by plumes of buoyant, hot ation over their vigorous opposition to material that arise in the deep mantle and punch Wegener’s theory of continental drift. -
Moho and Basement Depth in the NE Atlantic Ocean Based on Seismic Refraction Data and Receiver Functions
Downloaded from http://sp.lyellcollection.org/ by guest on September 27, 2021 Moho and basement depth in the NE Atlantic Ocean based on seismic refraction data and receiver functions THOMAS FUNCK1*, WOLFRAM H. GEISSLER2, GEOFFREY S. KIMBELL3, SOFIE GRADMANN4,O¨ GMUNDUR ERLENDSSON5, KENNETH MCDERMOTT6 & UNI K. PETERSEN7 1Geological Survey of Denmark and Greenland, Øster Voldgade 10, 1350 Copenhagen K, Denmark 2Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Am Alten Hafen 26, 27568 Bremerhaven, Germany 3British Geological Survey, Keyworth, Nottingham NG12 5GG, UK 4Geological Survey of Norway, Leiv Eirikssons vei 39, 7040 Trondheim, Norway 5Iceland Geosurvey, Grensa´svegi 9, 108 Reykjavı´k, Iceland 6UCD School of Geological Sciences, University College Dublin, Belfield, Dublin 4, Ireland 7Faroese Earth and Energy Directorate, Brekkutu´n 1, 110 To´rshavn, Faroe Islands *Correspondence: [email protected] Abstract: Seismic refraction data and results from receiver functions were used to compile the depth to the basement and Moho in the NE Atlantic Ocean. For interpolation between the unevenly spaced data points, the kriging technique was used. Free-air gravity data were used as constraints in the kriging process for the basement. That way, structures with little or no seismic coverage are still presented on the basement map, in particular the basins off East Greenland. The rift basins off NW Europe are mapped as a continuous zone with basement depths of between 5 and 15 km. Maximum basement depths off NE Greenland are 8 km, but these are probably underestimated. Plate recon- structions for Chron C24 (c. 54 Ma) suggest that the poorly known Ammassalik Basin off SE Greenland may correlate with the northern termination of the Hatton Basin at the conjugate margin. -
Short-Lived and Discontinuous Intraplate Volcanism in the South Pacific: Hot Spots Or Extensional Volcanism?
Review Geochemistry 3 Volume 4, Number 10 Geophysics 28 October 2003 GeosystemsG 1089, doi:10.1029/2003GC000533 G ISSN: 1525-2027 AN ELECTRONIC JOURNAL OF THE EARTH SCIENCES Published by AGU and the Geochemical Society Short-lived and discontinuous intraplate volcanism in the South Pacific: Hot spots or extensional volcanism? Anthony A. P. Koppers and Hubert Staudigel Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography, University of California, San Diego, La Jolla, CA 92093-0225, USA ([email protected]; [email protected]) Malcolm S. Pringle Argon Isotope Facility, Scottish Universities Environmental Research Center, Rankine Avenue, East Kilbride G75 0QF, UK ([email protected]) Jan R. Wijbrans Laboratory of Isotope Geology, Vrije Universiteit Amsterdam, De Boelelaan 1085 1081 HV Amsterdam, Netherlands ([email protected]) [1] South Pacific intraplate volcanoes have been active since the Early Cretaceous. Their HIMU-EMI- EMII mantle sources can be traced back into the West Pacific Seamount Province (WPSP) using plate tectonic reconstructions, implying that these distinctive components are enduring features within the Earth’s mantle for, at least, the last 120 Myr. These correlations are eminent on the scale of the WPSP and the South Pacific Thermal and Isotopic Anomaly (SOPITA), but the evolution of single hot spots emerges notably more complicated. Hot spots in the WPSP and SOPITA mantle regions typically display intermittent volcanic activity, longevities shorter than 40 Myr, superposition of hot spot volcanism, and motion relative to other hot spots. In this review, we use 40Ar/39Ar seamount ages and Sr-Nd-Pb isotopic signatures to map out Cretaceous volcanism in the WPSP and to characterize its evolution with respect to the currently active hot spots in the SOPITA region.