Deep Sea Drilling Project Initial Reports Volume 47 Part 2

Total Page:16

File Type:pdf, Size:1020Kb

Deep Sea Drilling Project Initial Reports Volume 47 Part 2 INDEX Acaeniotyle umbilicata Zone, 668 Background and objectives, Site 398, 26 Acoustic Bacterial, sulfate reduction, 733 anisotropy, 59, 585 activity, 44 basement, 86, 639 Base-of-slope province, 374 impedance, computation of, 625, Site 398, 63 Basement, 639 pseudologs, 623 Basins and Site 398, correlation between regional, 647 stratigraphy, 91, 639 Bedoulian group, 290 Site 398, 761 Bejaouaennsis Zone (MCi 23), 292 unit 3, nature of, 86 Belemnites, 55, 297 velocity, 585 Benthic, foraminifers, 729 Age of opening of North Atlantic, 28 assemblages, 293 Agglutinated foraminifers, 290, 294, 691 residual, 290, 293, 295 residual, 292 Betic system, 658 Algerianus Zone (Mci 21), foraminifers, 291 Biogenic activity, indexes of organic matter, 419 Alkalinity, 578 minerals, Lower Cretaceous sediments, 686 Alteration indexes, 543 Biostratigraphy, 69 Ammonites, 56, 75, 290, 297 Cenozoic foraminifers, 69, 255 Douvilleiceras mammilatum Zone, 362 Lower Cretaceous, 688 Euhoplites lautus Zone, 362 nannofossils, 327 loricatus Zone, 362 Bioturbation: See Burrows Hoplites dentatus Zone, 362 evidence for, 258 Lower Cretaceous, 361 Bitumen content, Hole 397 sediments, 543 systematic descriptions, 362 Black shale deposition, 30, 55, 56, 405, 437, 665, 667 Amorphous kerogen, 550 719 Ampere Bank, 659 analysis of, 472 Angola Basin, 575, 735 organic matter in, 719 Angular unconformity, 56, 93 Block-faulting, 93 Anistropy, degree of cementation, relationship to, 585 Bottom currents, 375, 380 Anomaly /, 639 temperatures, 511 MO, 639 water, formation of, Antarctic, 511 34, 95, 766 waters, low-oxygen conditions, 728 Anoxic conditions, 56 Bottom-current activity, 48, 729 Antarctic bottom water, formation of, 511 Bouma sequences, 53 Antarctica, ice formation on, 441 Broinsonia parca Zone, defined, 331 Anticlines, diapiric, 636 Burial depth and carbonate content, sound velocity re- Aptychus, 297, 404 lationship to, 646 Argo Formation, 28 Burrows, 41, 42, 54, 258, 419, 729 Assemblage-lithofacies relationship, lithologic sub-unit Chondrites, 36, 51, 381 Illb, 308 Helminthoides, 381 Sub-unit Ilia, 306 Mycellia, 36, 381 Ila, 300 Zoophycos, 37, 51, 381 lie, 303 Chiatozygus litterarius Zone, 76 lid, 304 Cabri Zone (Mci 19), 291 IVa, 309 Calcicalithina oblongata Zone, defined, 330, 76 IVb, 310 Calcite, origin of, 435 Unit V, 311 compensation depth, 385 Atlantic, opening of, 667 Calcium carbonate content, relationship to reflectors, Siliceous reproductivity, 49 590 subsidence and opening of, 674 Calpionellids, 289 Attapulgite, 52, 56 Campanian-Cenomanian hiatus, 51, 534 formation of, 437 Campanian/Maestrichtian boundary, 77 Authorship, responsibility for, 5 Cape Basin, 553, 575 Autochronous facies, 48 Carbon, Hole 398D, geochemistry of, 554 Azores-Gibraltar line, 768 Holes 397 and 397A, Geochemistry of, 553 777 isotope event, 489 stresses, 636 isotope data, 489 velocity, relationship to clay content, 589 13 data, isotopic unit, 509 wave velocities as a function of pressure, 587 14, isotopes from bulk carbonate samples, 493 Computation of acoustic impedances, 625 Lithologic unit 1, geochemistry of, 554 Condensed sedimentation, 294 2, geochemistry of, 555 Continental blocks, subsidence of, 93 3, geochemistry of, 555 Continental deposits, 636 4, geochemistry of, 561 fragmentation, geometry of initial, 28 Carbon-carbonate analyses, 16, 65 margin, tectonic setting, West Iberia, 753 Carbon-oxygen isotopes, effect of diagenesis on, 493 of Iberia, dominant structural trends, 753 Carbon-13 values, Cretaceous-Tertiary transition, margins, history of, 30 change in, 494 mechanisms to explain, formation and, evolu- post-Eocene, 494 tion of, 768 Carbonate bomb data, 13 rise province of passive margins, 374 compensation depth, 244, 297, 299 Contourite, 381 content, 535 Convoluted bedding, 53 sound velocity, relationship to burial depth Cooling, Cenozoic worldwide, 441 and, 646 Copper porphyrin, 573 cycles, 385 Core temperature, effect on velocity measurements, preservation, 45 585 samples, oxygen 18 and carbon 14, isotopes, 493 Correlation between regional basins and Site 398, 647 sedimentation and diagenesis, 732 of lithology with acoustics, Formation la, 647 Carbonification level, 695 lb, 647 Catagenesis, primary, 719 3, 647 Catinaster coalithus Zone, defined, 358 4, 647 Cementation, relationship to anistropy, 585 reflection profiles with, drilling results, 80 Cenomanian transgression, 636, 674 Correspondence analysis, aim of, 469 section, Site 398D, 404 Cretaceous, Black shales, 719 Cenomanian/Campanian unconformity, 527 foraminifers, 74, 289 Cenozoic compressional movements, 675 magnetic quiet zone, 766 foraminifers, biostratigraphy, 675 nannofossils, 76, 77, 329 nannofossils, 72 palynofacies, 453 objectives, 31 petroleum-generating capability of, 533 paleotemperatures, Site 398, 507 Sedimentary environments, Site 398, 719 palynology, 74 quiet zone, 639 sedimentary evolution, 48 sediments, lipid geochemistry of, 567 structural evolution, 651 nature and, origin of organic content, 529 sediments, diagenesis, 44 sapropelic, 529 sequence, 44 shales, geochemistry, 513 worldwide cooling, 441 mineral carbon, 513 Ceratolithus tricorniculatus Zone, defined, 359 organic carbon, 514 Charlie-Gibbs fracture zone, 95, 768 petrography, 523 Chiasmolithus danicus Zone, defined, 72, 331 Cretaceous-Tertiary boundary, 44 oamaruensis Zone, defined, 353 paleotemperature trends, 477 Chiastozygus litterarius Zone, defined, 74, 330 transition, change in carbon-13 values, 494 Chiphragmalithus alatus Zone, defined, 72, 352 Cretaceous/Paleocene boundary, foraminifers, 69 Chloroform extracts, 517 Cretaceous/Tertiary boundary, nannofossils, 77 Chlorophyll diagenesis, 571 Cretahabdulus crenulatus Zone, 74 Chondrites, burrows, 36, 51, 381 Cristobalite, origin of, 438 Chronostratigraphy, 289 Cross-laminations, 53 foraminifers, 237 Cruciellipsis curvillieri Zone, 76 Circulation changes, North Atlantic, 31 defined, 330 Clay content, compressional velocity, relationship to, Cruciplacolithus tennis Zone, defined, 72, 331 589 Current deposition, 646 Climatic and eustatic oscillations, 389 Cyclic association, 385 indicator, smectite, 441 bedding, rhythmic and, 48 oscillations, cyclic sedimentation as a result of, 48 sedimentation, 387 Clinoptilolite, origin of, 438 as a result of, climatic oscillations, 48 Compressional movements, Cenozoic, 675 Dark shales, 292, 297, 299, 302, 305 778 Debris flow, 48, 51, 53, 55, 384, 548 Edgari Zone, 79 deposits, 35, 388 Eiffelithus turriseiffeli Zone, 76 sedimentary structures, 411 defined, 330 Deep oceanic circulation, 674 Ellipsolithus macellus Zone, defined, 349 Deep-sea fan, 53, 405, Emiliania huxleyi Zone, defined, 359 environment, graded sequences, 405 Environmental conditions, reducing, 667 Degree of cementation, relationship to anisotropy, 585 Environments, changes in, 658 Delta systems, 56, 724 Eocene, foraminifers, 71 Deltaic progradation, 53 nannofossils, 72 Demagnetization, 602 paleotemperatures, 74 Diagenesis, carbonate sedimentation and, 732 reverse faults, 651 Cenozoic sediments, 44 sedimentary hiatus, 242 carbon-oxygen isotopes, effect of, 493 Eocene/Oligocene boundary, nannofossils, 73 Diagenetic modification, bearing on isotope data, 488 transition, 511 trends, oxygen-isotopic composition, 477 Ericsonia subdisticha Zone, defined, 353 Diapiric, anticlines, 636 Erosion, Formation 1, 646 Diaprisim, 665 Erosional surfaces, depth of, 653 salt, 764 Etio series, 573 Dictyomitra somphedia Zone, 688 Eugubina Zone, 296 Differential pelagic settling, 377 Euhoplites lautus Zone, 362 Dilution, 380 loricatus Zone, 362 Discoaster asymmetricus Zone, defined, 73, 74, 359 Eustatic oscillations, 389 binodosus Zone, defined, 349 Evaporites, 93, 735 brouweri Zone, defined, 359 Evaporitic sediments, 636 calcaris Zone, defined, 73, 358 series, 93 druggi Zone, defined, 358 Evolution of Continental margins, mechanisms to ex- exilis Zone, defined, 73, 358 plain, 768 hamatus Zone, defined, 358 facies, 387 kugleri Zone, defined, 73, 358 paleotemperatures, 508 lodoensis zone, defined, 72, 349 Exinitic palynofacies, 454 mohleri Zone, defined, 349 Expansion, oceanic, 658 multiradiatus Zone, defined, 72, 349 Facies association, 385 nodifer Zone, defined, 72, 352 units, 388 pentaradiatus Zone, defined, 359 Faeroe-Shetland shelf, 57 quinqueramus Zone, defined, 73, 359 Fan-shaped sedimentary features, 94 saipanensis Zone, defined, 352 Fasciculithus tympaniformis Zone, 72 sublodoensis Zone, defined, 72, 349 defined, 349 surculus Zone, defined, 73, 359 Faulted blocks, 93 Discontinuity, 421 Faults, 658 Dispersed organic matter (DOM), geochemistry of, 695 reverse, 671 Dissolution, 289, 380, 381 strike-slip, 757 effect on isotopic signal, 507 Ferreolensis Zone (Mci 20), 291 foraminifers, 255, 297 Fibrous clays, origin of, 435 Distal-type, graded units, 384 Flame structures, 42, 46 Doukala Formation, 28 Flaser lamination, 46 Douvilleiceras mammilatum Zone, 362 structure, 41 Downhole measurements, 80 Fluorescence analyses, 69 Drilling results, correlation of reflection profiles with, Foraminiferal lysocline, 45 80 Foraminifers, agglutinated, 290, 294, 691 characteristics, Site 398, 5, 63 Algerianus Zone (Mci 21), 291 deviation, effect on paleomagnetic results, 604 Assemblages, classification of, 287 operations, 32 Bedoulian group, 290 DPEP/etio ratio, 573 Bejaouaennsis Zone (Mci 23), 292 Early Cretaceous, nannofossils, 76 benthic, 729 Cretaceous rifting, 649 assemblages, 293 tension tectonics, 666 residual, 295 Cretaceous-early Miocene unconformity, 533 biostratigraphy, 237, 255 Cretaceous-Miocene
Recommended publications
  • The Long-Term Evolution of the Congo Deep-Sea Fan: a Basin-Wide View of the Interaction Between a Giant Submarine Fan and a Mature Passive Margin (Zaiango Project)
    The Congo deep-sea fan: how far and for how long? A basin-wide view of the interaction between a giant submarine fan and a mature passive margin Zahie Anka 1,*, Michel Séranne 2,**, Michel Lopez 2, Magdalena Scheck-Wenderoth 1, Bruno Savoye 3,†. 1. GFZ German Research Centre for Geosciences. Telegrafenberg, 14473 Potsdam, Germany. 2. CNRS-Université Montpellier II. cc 060, Geosciences Montpellier. 34095 Montpellier, France. 3. IFREMER, Geosciences Marines, BP 70 — 29280 Plouzané, France. (*) [email protected] (**) [email protected] (†) deceased 1.- Introduction The Congo deep-sea fan is one of the largest submarine fan systems in the world and one of the most important depocentre in the eastern south Atlantic. The present-day fan extends over 1000 km offshore the Congo-Angola continental margin and it is sourced by the Congo River, whose continental drainage area is the second largest in the world (3.7 106 km²) (Droz et al., 1996) (Fig.1). There is a direct connexion between the river’s drainage basin and the deep basin through an impressive submarine canyon, which cuts down about 950 m at the shelf-break and more than 1300 m at 100 km offshore the coastline (Babonneau et al., 2002). Hence, the direct transfer of terrigenous material onto the abyssal plain takes place through the canyon, by-passing the shelf and upper slope. The submarine fan covers a surface of about 300,000 km² and contains at least 0.7 Mkm³ of Tertiary sediments (Anka and Séranne, 2004; Droz et al., 2003; Savoye et al., 2000).
    [Show full text]
  • SÉRANNE, M., and ANKA, Z., 2005
    ARTICLE IN PRESS Journal of African Earth Sciences xxx (2005) xxx–xxx www.elsevier.com/locate/jafrearsci South Atlantic continental margins of Africa: A comparison of the tectonic vs climate interplay on the evolution of equatorial west Africa and SW Africa margins Michel Se´ranne *, Zahie Anka UMR 5573 Dynamique de la Lithosphe`re, CNRS/Universite´ Montpellier 2, 34095 Montpellier cedex 05, France Received 5 February 2005; accepted 18 July 2005 Abstract Africa displays a variety of continental margin structures, tectonic styles and sedimentary records. The comparative review of two representative segments: the equatorial western Africa and the SW Africa margins, helps in analysing the main controlling factors on the development of these margins. Early Cretaceous active rifting south of the Walvis Ridge resulted in the formation of the SW Africa volcanic margin that displays thick and wide intermediate igneous crust, adjacent to a thick unstretched continental crust. The non-vol- canic mode of rifting north of the Walvis ridge, led to the formation of the equatorial western Africa margin, characterised by a wide zone of crustal stretching and thinning, and thick, extensive, syn-rift basins. Contrasting lithologies of the early post-rift (salt vs shale) determined the style of gravitational deformation, whilst periods of activity of the decollements were controlled by sedimentation rates. Regressive erosion across the prominent shoulder uplift of SW Africa accounts for high clastic sedimentation rate during Late Creta- ceous to Eocene, while dominant carbonate production on equatorial western Africa shelf suggests very little erosion of a low hinterland. The early Oligocene long-term climate change had contrasted response in both margins.
    [Show full text]
  • Sea Experience in Developing Countries
    Chapter 6 SEA EXPERIENCE IN DEVELOPING COUNTRIES Increasingly, developing countries are experimenting with SEA and some have SEA-type approaches and elements in place already. There is also considerable experience with using a variety of strategic planning processes that display many of the characteristics of SEA (para SEA). We focus first on SEA in southern Africa where a dedicated regional workshop on SEA was organised to feed into this review (SAIEA 2003a), followed by sections covering francophone Africa, the rest of sub-Saharan Africa, Latin America, Asia and elsewhere. But our survey of this field represents no more than a preliminary reconnaissance. Selected examples of SEA and para SEA illustrate some of the indigenous approaches that have been adopted. These are less common than SEAs promoted and funded by development assistance agencies (which are reviewed in Chapter 4). In most cases where formal SEA has been undertaken in developing countries, the basic aim and approach has mirrored that in the north – namely to identify the environmental consequences (and associated social and economic effects) of existing, new or revised policies, plans and programmes. These represent only a small number of the broad family of SEA approaches. But they are a highly visible sub-set of the large suite of informal or para-SEAs which form part of development policy-making, land use planning or resource management. No strict boundaries can be drawn for this latter area of application. Only the more evident SEA type elements and approaches are introduced in this chapter. Nevertheless, they indicate the scope and diversity of the extended SEA family in developing countries, where political and economic realities constrain what can be done.
    [Show full text]
  • Hafnium and Neodymium Isotopes in Surface Waters of the Eastern Atlantic Ocean: Implications for Sources and Inputs of Trace Metals to the Ocean
    Available online at www.sciencedirect.com Geochimica et Cosmochimica Acta 74 (2010) 540–557 www.elsevier.com/locate/gca Hafnium and neodymium isotopes in surface waters of the eastern Atlantic Ocean: Implications for sources and inputs of trace metals to the ocean J. Rickli a,*, M. Frank b, A.R. Baker c, S. Aciego a, G. de Souza a, R.B. Georg d, A.N. Halliday d a ETH Zurich, Institute for Isotope Geochemistry and Mineral Resources, Clausiusstrasse 25, CH-8092 Zurich, Switzerland b IFM-GEOMAR, Leibniz Institute of Marine Sciences, 24148 Kiel, Germany c School of Environmental Sciences, University of East Anglia, Norwich NR4 7TJ, UK d Department of Earth Sciences, University of Oxford, Parks Road, Oxford OX1 3PR, UK Received 14 January 2009; accepted in revised form 30 September 2009; available online 7 October 2009 Abstract We present hafnium (Hf) and neodymium (Nd) isotopic compositions and concentrations in surface waters of the eastern Atlantic Ocean between the coast of Spain and South-Africa. These data are complemented by Hf and Nd isotopic and con- centration data, as well as rare earth element (REE) concentrations, in Saharan dust. Hafnium concentrations range between a maximum of 0.52 pmol/kg in the area of the Canary Islands and a minimum value of 0.08 pmol/kg in the southern Angola Basin. Neodymium concentrations also show a local maximum in the area of the Canary Islands (26 pmol/kg) but are even higher between ~20°N and ~4°N reaching maximum concentrations of 35 pmol/kg. These elevated concentrations provide evidence of inputs from weathering of the Canary Islands and from the partial dissolution of dust from the Sahara/Sahel region.
    [Show full text]
  • Deep Sea Drilling Project Initial Reports Volume 40
    28. LEG 40 RESULTS IN RELATION TO CONTINENTAL SHELF AND ONSHORE GEOLOGY William G. Siesser, Department of Geology, University of Cape Town, Rondebosch, South Africa INTRODUCTION tion of basins; instead a sediment wedge has prograded seaward in a deltaic fashion (Scrutton and Dingle, This study compares and contrasts the sedimentary 1974). However, there is some suggestion that history of the onshore coastal region and the continen- marginal-fracture zones striking perpendicular to the tal shelf along the west coast of South Africa, South coast have acted as lines of differential subsidence, thus West Africa, and Angola with that of the outer con- exercising some control over the movement of tinental margin of those countries (Figure 1), as shown sediments parallel to the coast (Scrutton and Dingle, by Leg 40 drilling. 1974). This situation is in contrast to the Cuanza Basin of Geologic Setting: Mesozoic and Tertiary Sedimentation Angola, where sedimentation has been controlled by a Southern Africa underwent its last orogenic phase marginal basement plateau, a number of basement during the Triassic, raising up the Cape Fold Belt. highs, and salt structures (Scrutton and Dingle, 1974). Although no further orogenies occurred, southern Africa remained a high continental mass throughout Onshore the Mesozoic and Cenozoic owing to repeated epeiro- Only two Cretaceous exposures have been reported genic uplift. Epeirogenesis had a characteristic and between Cape Agulhas and the Kunene River. The repeated pattern: maximum uplift occurred in a zone southernmost is a deposit of nonmarine clayey sands near the coastal margin (somewhat seaward of what is (with calcareous concretions) containing bones of the now the Great Escarpment), resulting in a steep dinosaur Kangnasaurus coetzeei, calcified and silicified seaward tilting on the outer side and a gentler inland wood, and streaks of lignite (Rogers, 1915).
    [Show full text]
  • Sea Experience in Developing Countries
    Chapter 6 SEA EXPERIENCE IN DEVELOPING COUNTRIES Increasingly, developing countries are experimenting with SEA and some have SEA-type approaches and elements in place. There is also considerable experience of using a variety of strategic planning processes which display many of the characteristics of SEA (para SEA). We focus first on SEA in southern Africa where a dedicated regional workshop on SEA was organised to feed into this review (SAIEA 2003a), followed by sections covering francophone Africa, the rest of sub-Saharan Africa, Latin America, Asia and elsewhere. Selected examples of SEA and para SEA illustrate some of the indigenous approaches that have been adopted. These are less common than SEAs promoted and funded by development assistance agencies (which are reviewed in Chapter 4). In most cases where formal SEA has been undertaken in developing countries, the basic aim and approach has mirrored that in the north – namely to identify the environmental consequences (and associated social and economic effects) of existing, new or revised policies, plans and programmes. 6.1 SEA in Southern Africa1 EIA is now used extensively in most countries in southern Africa. However, many of the governments tend to be ad hoc in their planning and, as a result, EIA is often regarded as an ‘add on’ process “that gets done ‘later on’, after the government, board of directors or other body has decided that the intended initiative is viable and thus worthy of detailed planning” (Tarr, 2003). In recent years, there has been rapid progress in the formulation of policies, legislation and guidelines for EIA (SAIEA 2003b).
    [Show full text]
  • Formation and Collapse of the Kalahari Duricrust ['African Surface
    Formation and Collapse of the Kalahari Duricrust [‘African Surface’] Across the Congo Basin, 10 with Implications for Changes in Rates of Cenozoic Off-Shore Sedimentation Bastien Linol, Maarten J. de Wit, Francois Guillocheau, Michiel C.J. de Wit, Zahie Anka, and Jean-Paul Colin{ 10.1 Introduction margins, and to the east by the East African Rift System (EARS). Their relatively flat interior is covered by an exten- The Congo Basin (CB) of central Africa lies at about 400 m sive Upper Cretaceous-Cenozoic succession of sand dunes, above mean sea level (amsl), and is linked to the south, pan-lacustrine sediments and alluviums with hard-caps across a central African drainage divide, to the high interior (duricrusts) of calcrete, silcrete and ferricrete, collectively Kalahari Plateau (KP) at ca. 1,100 m amsl (Fig. 10.1). The named the Kalahari Group (SACS, 1980). This succession CB and KP are flanked by distinct marginal escarpments reaches a maximum thickness of about 500 m, but across along the South Atlantic and southwest Indian Ocean southern and central Africa is generally less than 100 m thick, representing one of the world’s most extensive, long- lived condensed stratigraphic sequences. The Kalahari Group directly overlies Precambrian base- ment of the Kalahari and Central African Shields (Fig. 10.1b), late Paleozoic to mid-Mesozoic sequences of {Author was deceased at the time of publication. the Karoo Supergroup including Lower Jurassic flood basalts in southern Africa, dated at 178–183 Ma (the B. Linol (*) AEON-ESSRI (African Earth Observatory Network – Earth Stormberg Group; Jourdan et al.
    [Show full text]
  • Back Matter (PDF)
    Index Page numbers in bold refer to tables; those in italic refer to figures Abidjan Basin 102, 117, 124, 126-7,242,259 shales 26, 68-70, 142, 153-66, 296-300, 314, 407 Abrolhos massif 133-4, 138-9 South African Margin 153-66, 296 Acarafi Basin 134,141 tectonics 63-72, 104-24, 135,141-4, 303-18,441 aeolian sediments 1, 57, 8%90, 92, 105, 142 Aptian Salt Basin 8,107-116, 181-8,192-4,294-300 Namibia 159-60, 325, 347-62, 367 79 Aptian-Albian 70-2, 307-8 Southern African Margin 159-60 Aqua Salada Fauna 267-79 Afar 87, 94 Araguaia River 32-3 Afro-Brazilian Depression 133-49 Araripe Basin 56-8, 64-71,134-5 Agadir Basin 215,223 Argentine 1-8, 293-6, 338,388 agglutinated foraminfera 203,205,209-15, 218 Argilles Vertes 25-7 Cabinda 267-79 Ascension Fracture Zone 79-80, 135,140, 304-5 Agulhas Bank 405,421 asymmetric grabens 33, 61-7, 71-2, 404 Agulhas Current 327 asymmetric rifts 12, 23-7, 138-9, 144, 431 Agulhas-Falkland Transform Fault 102, 105,158,163, Rio Muni 305, 311 294-5 Atlantic Hinge Zone 8, 12-27, 36-7 Falklands 405-6, 409-11, 415-22, 435-6 Atlantic Margin 8, 41-53 Alagoas Hinge 15-17, 36, 80,158, 420 Atlantic Rift 53-72 and see break-up Albacora Field 6, 145-7 Austral Basin 163,293-6, 428,435-6 Albian 51,124-8,305-18, 441 Autseib Linement 382-401 break-up 71,105, 135, 141,243-61,295-300 Cabinda 268, 283-92, 468 back-arc 420-2 micrites 182-3, 190-4 Bahia Basin 135, 141,170-8 shales 142-8, 182-94, 223-39, 296-300 Barreirinhas Basin 102, 117, 126, 244 tectonics 70-2, 104-5, 108-24, 135-40 tectonics 59,134-5,137, 141,148 Albian-Cenomanian
    [Show full text]
  • Congo River Sand and the Equatorial Quartz Factory
    Earth-Science Reviews 197 (2019) 102918 Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev Congo River sand and the equatorial quartz factory T ⁎ Eduardo Garzantia, , Pieter Vermeeschb, Giovanni Vezzolia, Sergio Andòa, Eleonora Bottia, Mara Limontaa, Pedro Dinisc, Annette Hahnd, Daniel Baudete, Johan De Gravef, Nicole Kitambala Yayag a Laboratory for Provenance Studies, Department of Earth and Environmental Sciences, University of Milano-Bicocca, 20126 Milano, Italy b London Geochronology Centre, Department of Earth Sciences, University College London, London, WC1E 6BT, UK c Department of Earth Sciences, MARE – Marine and Environmental Sciences Centre, University of Coimbra, Portugal d MARUM Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany e Geodynamics & Mineral Resources, Royal Museum for Central Africa (RMCA), Leuvensesteenweg 13, 3080 Tervuren, Belgium f Department of Geology and Soil Science (WE13), MINPET, Ghent University, Krijgslaan 281/S8, WE13, B-9000 Gent, Belgium g CRGM Centre de Recherches Géologiques et Minières, 44, Av. de la Démocratie, Kinshasa-Gombe, Democratic Republic of Congo ARTICLE INFO ABSTRACT Keywords: A never solved problem in sedimentary petrology is the origin of sandstone consisting exclusively of quartz and Provenance analysis most durable heavy minerals. The Congo River offers an excellent test case to investigate under which tectonic, Equatorial weathering geomorphological, climatic, and geochemical conditions pure quartzose sand is generated today. In both upper U-Pb zircon geochronology and lowermost parts of the catchment, tributaries contain significant amounts of feldspars, rock fragments, or Zircon weatherability moderately stable heavy minerals pointing at the central basin as the main location of the “quartz factory”.
    [Show full text]
  • Download This PDF File
    Acta Geologica Polonica, Vol. 48 (1998), No. 1, pp. 43-106 Facies, stratigraphy and diagenesis of Middle Devonian reef- and mud-mounds in the Mader (eastern Anti-Atlas, Morocco)1 BERND KAUFMANN Institut für Geologie und Paläontologie der Universität Tübingen, Sigwartstr. 10, D-72076 Tübingen, Germany. E-mail: [email protected] ABSTRACT: KAUFMANN, B. 1998. Facies, stratigraphy and diagenesis of Middle Devonian reef- and mud-mounds in the Mader (eastern Anti-Atlas, Morocco). Acta Geol. Polon., 48 (1), 43-106. Warszawa. During the Devonian, the eastern Anti-Atlas formed a part of the northwestern continental margin of Gondwana which was a mid-latitudinal (30-40°S), temperate-water carbonate province. In the Mader region, ten carbonate mounds (one reef-mound and nine mud-mounds), distributed over five discrete localities, are intercalated within a 200-400 m thick Middle Devonian succession. The arid climate of the northwestern margin of the Sahara has exhumed these mounds which display perfectly their origi- nal morphologies and relations to off-mound lithologies. The carbonate mounds of the Mader area consist of massive, stromatactis-bearing boundstones (wackestones and floatstones in a purely descriptive manner) with the bulk of the mound volume con- sisting of fine-grained carbonate (microspar). High accumulation rates (0.2-0.8 m/1000 a), purity of mound carbonates (> 95% CaCO3) and homogeneous Mg-calcite mineralogy strongly argue for in situ carbonate production by microbial (cyanobacterial/bacterial) communities. In addition, other indica- tions (calcified cyanobacteria in the immediate neighbourhood of stromatactis fabrics, dark crusts sur- rounding stromatactis fabrics and alignment of stromatactis fabrics parallel to the accretionary mound surfaces) suggest a close relationship between stromatactis formation and carbonate production.
    [Show full text]
  • Deep Sea Drilling Project Initial Reports Volume 74
    9. CRETACEOUS-TERTIARY PLANKTONIC FORAMINIFERS FROM THE SOUTHEASTERN ATLANTIC, WALVIS RIDGE AREA, DEEP SEA DRILLING PROJECT LEG 741 Anne Boersma, Microclimates, Inc., Box 404, RR 1, Stony Point, New York ABSTRACT Planktonic foraminifers were studied from the > 149 µm fractions of Cretaceous and Cenozoic sediments at DSDP Sites 525, 526, 527, 528, and 529, all clustered in the southernmost Angola Basin and central Walvis Ridge area of the southeastern Atlantic. Faunas were commonly mixed by consistent slumping in the Maestrichtian and, to a lesser de- gree, in the Paleocene. Contamination that is presumed to be due to downhole coring emplacement of coarse-fraction drilling sands was common in thte Miocene of Sites 525 and 528, particularly in the mid-Miocene (Zones NI 1-N13). Spe- cies ranges presumed to be anomalous in these intervals, therefore, are frequent. Cretaceous sediments were interlayered with basalt and/or altered by contact with basalt at all but Site 529. Incon- sistency between foraminiferal and nannofossil zonations and paleomagnetic results through most of the Maestrichtian at all sites is attributed to consistent slumping of sediment coarse fractions, which include most of the foraminifers. Paleocene sediments are moderately well preserved at Sites 525, 527, 528, and 529, but the sections are incomplete. Only shallow-water carbonates with some larger foraminifers were attributed to the Paleocene (Manivit, this volume) in Hole 526C. At three sites, 525, 527, and 528, good, apparently continuous Paleocene/Eocene boundary sections were recovered. The Eocene was recovered at all sites, but is incomplete because of dissolution near the CCD at Sites 528 and 527, typical South Atlantic mid to late Eocene dissolution and recrystallization at Sites 525 and 529, and lack of index fossils in the shallow-water carbonates at Site 526.
    [Show full text]
  • A V~*» the URANIUM GEOLOGY and TECTONIC CORRELATION
    •••, A v~*«^» í f >-v ,— / PER-58 THE URANIUM GEOLOGY AND TECTONIC CORRELATION BETWEEN THE AFRICAN AND LATIN AMERICAN CONTINENTS by P.D. Toens J.P. le Roux C.J.H. Hartnady W.J. van Biljon /| ATOMIC ENERGY BOARD _i, j Pelinclaha T> J! PRETORIA x | Republic of South Africa October 1980 8 .ii. ::iii!!:imi:::: gjpji, lip£.l.^....diyiii^..,».M!i» *ltji|ill I «•••*«••• •••«•If*III(**««*}«atja•*••••**•••*•***<*••••• «•(•I<>«lil«ll»»"<'->1 I.. !!::::i::!ii:J:i:: PER-58 THE URANIUM GEOLOGY AND TECTONIC CORRELATION BETWEEN THE AFRICAN AND LATIN AMERICAN CONTINENTS by P.D. Toens* J.P. le Roux* C.J.H. Hartnady** W.J. van Biljon*** *Geo1ogy Division POSTAL ADDRESS: Private Bag X256 PRETORIA 0001 **University of Cape Town ***Rand Afrikaans University PELINDABA October 1980 [OnÁQÍnaíly pfiuzntíd cu> an intoxÁm Kzpoht by thz South A^fvican Walking Gnoixp to thz IAEA Consultants' Mz&ting, Vienna, JLU.IJ 1980) ISBN 0 86960 720 0 PER-58-1 CONTINENTS, LIKE PEOPLE, CAW MO LONGER BE STUV1EV EFFECTIVELY IN/ ISOLATION. PER-58-2 MIEVATTIH8 CONTENTS Page ABSTRACT 1. GENERAL STATEMENT 7 2. INTRODUCTION 8 3. CORRELATION OF METALLOGENIC PROVINCES 11 4. PRE-DRIFT RECONSTRUCTION OF WEST GONDWANALAND 14 4.1 Accuracy and Precision of Reconstruction 14 4.2 Basic Review of Previous Reconstructions 15 4.3 Proposed New Reconstruction 16 5. RELATIONSHIP BETWEEN MAJOR URANIUM METALLOGENIC 18 PROVINCES AND GEOTECTONIC PROVINCES 6. PERMO-TRIASSIC GONDWANA BASINS 21 6.1 Tectonic Setting 21 6.2 Description of Uranium Deposits in Gondwana 30 (Karoo) Basins 6.2.1 Main Karoo Basin 30 6.2.2 Waterberg Basin 32 6.2.3 Botswana Basin 32 6.2.4 Limpopo Basin 33 6.2.5 Mozambique Basin 33 6.2.6 Etjo Basin 33 6.2.7 Ovambo Basin 33 6.2.8 Mid-Zambezi Basin 34 6.2.9 Lower-Zambezi Basin 35 6.2.10 Barotse Basin 35 6.2.11 Angola Basin 36 6.2.12 Luano-Luangwa Basin 36 6.2.13 East African Basin 36 6.2.14 Rukwa Basin 36 6.2.15 Congo Basin 37 6.2.16 Gabon Basin 37 6.2.17 Parana Basin (Southern Brazil) 37 6.2.18 Callingasta-Uspallata Basin (Argentina) 37 7.
    [Show full text]