DOCSLIB.ORG

Dsdp42pt2 Index.Pdf

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Dsdp42pt2 Index.Pdf INDEX Absorption chromatography, bitumoids, 683 Azov, Sea of, Caspibraackish ostracodes from, 1039 Acritarchs, 993 Background and objectives, Site 379, 30 Aegean Sea, present-day salinity values, 643 Site 380, 120 Afig Formation, 1208 Site 381, 294 Age determinations based on pollen, 515 Bacteria, sulfate-reducing, 767 radiocarbon values, 627 Bacterial activity, carbon dioxide reduction, 673 varves, 483 controlled by methane production, 649 Algerian continental margin, 1181 Bacterial densities in Black Sea sediments, 769 Algerian shelf, tectonic activity, 1181 Bacterial sulfate reduction, depositional environment of, 625 Alkaline metal content, Black Sea sediments, 597 Balearic Basin, 1100 Alkanes, 697 Barite, 423 Alloisoleucine-isoleucine ratios, dependence on deposi- Bathymetry, Black Sea, 360, 1043 tional environment, 700 Belaya River, 413 Alpha cold period, 30, 41, 147, 299, 997 Benthic foraminifers from sediments of western shelf, Black Alpha glacial stage, 133, 513, 516 Sea, 783 Aluminosilicates, Hole 379A, 531 Benthic foraminifers, as salinity indicators, 493 Amino acid abundances, effect of depth on, 699 Hole 380, 146 Effects of reducing and oxidizing environment on, 699 Site 381, 298 Hole 379A, 699, 704, 727 Benthic ostracodes from Lake Erie, 1039 Hole 380A, 699 Benthic ostracodes from Great Lakes, 1039 Site 381, 699, 727 Benzene, 673 temporal variations in, 699 Bering Sea sediments, 744 Amino acids, 725, 1176 Bet Guvrin formation, 1197 Amino acids in Black Sea sediment samples, 698 description of, 1201 Amorphous silica, geochemistry of, 585 Bet Guvrin sedimentary cycle, 1199 Analytic techniques, major elements, 527 Bet Nir conglomerate, 1208 minor elements, 527 Beta cold period, 30, 41, 299, 513 Analytical procedures, organic geochemistry of sediments, Betty warm period, 30 755 Biostratigraphic datum levels, Israel, 1197 strontium concentrations in sediments, 608 Biostratigraphy, Hole 380, 146 Anatolian Fault, 1046 method of, Leg 42B, 12 Andesite tuffs dredged on submarine Arkhangelsky Ridge, Site 379, 37 469 Site 381, 298 Andesitic tuffs dredged in the Sinopian area, 471 Biostratigraphy summary, Black Sea, 17 Apulian-Agean-Anatolian blocks, 1077 Bioturbate textures, 504 Arab-African plate, 1077 Bioturbation, 383 Arabian Platform, paleogeographic reconstruction, second Bituminological studies, Site 379, results of, 690 erosional phase, 1204 Bitumoids, 726 transgression of the Ziglag Reef over, 1208 absorption chromatography, 683 Arabian Platform, 1199, 1214 Black Sea, 683 Emergence of, 1201, 1217 carbonate content, 683 Aragonite, 382, 385, 452, 462 column chromatography, 724 genesis features, 583 diagenesis, 727 inorganically precipitated, 34 gas chromatography, 727 Aragonite precipitation, 512, 618 gas-liquid chromatography, 683 Aral Lake, 1017 IR-spectrometry, 683 Aral Sea, 487 physical properties, Site 379, 683 Ardana-Kalogrea Formation, 1186 Site 379, composition of, 684 Arkhangelsky Ridge, dredging results from, 469 UV-spectrometry, 683 Asphaltenes, 727 Bitumosity, degree of in samples from Hole 379A and Site Athalassa formation, 1186 381, 727 Atlas Mountains, 1181 Black Sea, Atomic-absorption spectroscopy studies, 375 bathymetry, 360, 1043 Authigenic mineralogical forms of iron (total), 723, 726 benthic foraminifers from sediments of western shelf, Authorship, responsibility for, 6 783 1231 biostratigraphy summary, 17 sedimentary framework, 359 bitumoids, 683 sedimentation rates, 1097 black shale sedimentation, 510 seismic activity, 1046 bottom sediments of, 627 seismic reflection profiles, 1044, 1141 Bouguer gravity anomaly in, 1044 stratigraphic classification schemes, 17 carbonate varves in, 135 stratigraphy, 17, 361, 1167 chemical sedimentation, 510 stratigraphy problems, 1151 diatom varves from, 137 structural setting, 1077 diatoms, 1160 sulfur, 1172 distribution of Recent sediments, 1079 tectonic setting of, 1141 foraminifers, 1158 terrigenous sedimentation, 513 forestation of area around, 956 thermocline, 134 geologic history, 520 varves, 499, 1158 geological setting, 1043 Black Sea area, regional geology, 359 geophysical and geological setting of, 1141 Black Sea Basin, 1065 geophysical surveys, 1154 subsidence of, 1147 gravity studies, 1044 Black Sea cores, chronostratigraphical correlation, 515 halocline, 730 Black Sea drainage area, 359 heat flow, 1046, 1099 Black Sea during the Pleistocene glacial fluctuations, his- heavy minerals, 1172 tory of, 638 history of, 1147 Black Sea during Quaternary, paleoclimate, 519 Holocene varve chronology, 499 Black Sea glacial stages, based on preliminary paleomagne- hydrocarbon potential, 1177 tic results, 519 hydrography, 360 Black Sea history as determined by diatoms, 856 inorganic geochemical studies, 1169 Black Sea region, evolution of vegetation, 957 lacustrine environment, 373 Black Sea, salinization of, 628 lacustrine phase, 3, 1043 Black Sea sedimentation, lagoonal model, 510, 514 lacustrine sedimentation, 509 Role of Bosporus sill, 514 late Cenozoic, paleogeography of, 903, 912 Black Sea sediments, 360, 707, 765, 1155 late Cenozoic history of, 1141 alkaline metals content, 597 lithostratigraphy, 413, 495, 1141 bacterial densities in, 769 magnetics, 1046 boron content, 598 major prograding systems, 1079 carbon dioxide, 661 major rivers draining into the, 499 cobalt content, 589 marine transgression, 955, 1001 compared to Green River oil shale, 763 molluscs, 1159 copper content, 590 nannofossils, 1158 electrical resistivity measurements, 1125 Neoeuxinian epoch, 632 geochemistry of carbonates, 563 objectives for drilling, 3, 1149 hafnium content, 597 origin, 1046, 1098, 1100, 1155 hydrocarbon gases, 661 origin and geological history of, 1085 hydrolysate elements content, 593 ostracodes, 1158 interstitial water, 1174 paleontology, 1158 lithofacies, 383 paleosalinity, 730, 844,1148 lithofauna, 373 paleotemperature, 851 manganese content, 588 palynomorph distribution, 997 mineralogy, 360, 373 periodic chemical sedimentation, 513 molybdenum content, 590 petroleum-generation potential of late Cenozoic sedi- nickel content, 589 ments from, 729 nickel porphyrins, 707 physiographic provinces of, 1043 paleosalinity, 641 Playa Lake stage of, 643 phosphorus content, 597 Pleistocene isolation of, 637 radiocarbon ages, 483 pollen and spores, 1159 sediment color, 382 pH of surface waters, 843 sediment structures, 382 regime of, 3 selenium content, 591 salinity, 614, 627 tantalum content, 597 salinity changes of water, 536 thorium content, 594 sediment accumulation rates, 123, 499, 514, 1043. tin content, 594 1069, 1082, 1097, 1158, 1168 tungsten content, 591 sediment thickness, 1149 Black Sea surface water, depletion in oxygen-18 relative to sedimentary environment, 373 SMOW, 617 1232 Black shales, 828 Caucasus, 518 Black Sea, 510 source of sediments, Site 379, 657 Paratethys, 522 Caucasus Mountains, 1043, 1046 Blue-green algae, 766 Ceaudian Basin, 1017 Boron content, Black Sea sediments, 598 Celia warm period, 30 Bosporus Strait, 120, 638, 1043, 1065, 1094, 1149 Cheliff interior basin, 1181 sill depth of, 30, 373 Chemical gradient, interstitial water, 650 role of in Black Sea sedimentation, 514 Chemical sedimentation, 493 Bosporus area, foraminifers from sediments near, 783 Black Sea, 510, 835 Bosporus mineralogical province, 418 Chemistry, interstitial water, 649 Bosporus petrographic province, 422 Chesapeake Bay, sediments of, 513 Bosporus province, 361 Chlorin concentration, decrease with depth, Site 379, 708 Bouguer gravity anomaly in Black Sea, 1044 Hole 380, 710 Bromide in interstitial water Chlorin diagenesis, 713 Site 381, 635 Chlorine/bromine ratio, Holes 380/380A, 648 Site 380, 633 Site 380, 633 Bromine, Hole 379A in interstitial water, 632 Chlorine/bromine ratio, Site 381, 635 methods of analyses, 631 Chlorinity values, related to Pleistocene glaciation, 641 Brunhes/Matuyama boundary, 518, 1069 Chlorins, Site 147, mass spectrometry analyses, 708 Burrows, 32, 388 Site 379, mass spectrometry analyses, 708 described, 504 Chronostratigraphic analysis, palynological evidence, 1142 Butanes, 661 correlation Black Sea sites, 515, 1142 Butylanes, 51 Chronostratigraphy, diatoms, 1145 C-13 measurements, 1174 dinoflagellates, 1145 Calcite, 382 nannofossils, 1142 genesis features, 581 Chrysophyta cysts, indicators of desiccation, 834 high-magnesian, 382 Cimmerian orogeny, 1077 precipitation, 512 Clathrate, 679 Carbon, geochemistry of, Legs 42A and 42B, 717 Climate indicators, palynomorphs, 489 Carbon dioxide, Black Sea sediments, 661 Climatic changes, correlation of, 518 sources in sediment, 650 Climatic optimum, 618 Carbon dioxide reduction, bacterial activity, 673 Cobalt content, Black Sea sediments, 589 Carbon isotopes, head space methane, 667 Column chromatography, bitumoids, 724 Carbon-14, 1173 sugars from Black Sea sediment samples, 702 Carbon-carbonate analyses, method of, 9 Cooling effects of Northern Hemisphere glaciation on Gulf Carbon-13 content, Lipids, 752 of Mexico region, 516 lipid and kerogen fractions, 718 Copper content, Black Sea sediments, 590 lipid fraction, Site 380, 718 Core disturbance, Leg 42B, 8 Carbon-14 age determinations, Site 380, 627 Core handling, Leg 42B, 7 Vityaz 4754, 627 Correlation between sites, diatoms, 832 Carbon/nitrogen ratios, Hole 379A, 704 and seismic reflection data, 1079 Carbonate content, bitumoids, 683 Correlation of climatic changes, 518 equilibrium system, 649 lithologic units, 495 fractions, strontium content of, 612 Cretaceous black shales, Site 381, 756 genesis features, 581 Crimea, 1046, 1147 sediment analyses,
Load more

Recommended publications
  • The Last Maximum Ice Extent and Subsequent Deglaciation of the Pyrenees: an Overview of Recent Research
    Cuadernos de Investigación Geográfica 2015 Nº 41 (2) pp. 359-387 ISSN 0211-6820 DOI: 10.18172/cig.2708 © Universidad de La Rioja THE LAST MAXIMUM ICE EXTENT AND SUBSEQUENT DEGLACIATION OF THE PYRENEES: AN OVERVIEW OF RECENT RESEARCH M. DELMAS Université de Perpignan-Via Domitia, UMR 7194 CNRS, Histoire Naturelle de l’Homme Préhistorique, 52 avenue Paul Alduy 66860 Perpignan, France. ABSTRACT. This paper reviews data currently available on the glacial fluctuations that occurred in the Pyrenees between the Würmian Maximum Ice Extent (MIE) and the beginning of the Holocene. It puts the studies published since the end of the 19th century in a historical perspective and focuses on how the methods of investigation used by successive generations of authors led them to paleogeographic and chronologic conclusions that for a time were antagonistic and later became complementary. The inventory and mapping of the ice-marginal deposits has allowed several glacial stades to be identified, and the successive ice boundaries to be outlined. Meanwhile, the weathering grade of moraines and glaciofluvial deposits has allowed Würmian glacial deposits to be distinguished from pre-Würmian ones, and has thus allowed the Würmian Maximum Ice Extent (MIE) –i.e. the starting point of the last deglaciation– to be clearly located. During the 1980s, 14C dating of glaciolacustrine sequences began to indirectly document the timing of the glacial stades responsible for the adjacent frontal or lateral moraines. Over the last decade, in situ-produced cosmogenic nuclides (10Be and 36Cl) have been documenting the deglaciation process more directly because the data are obtained from glacial landforms or deposits such as boulders embedded in frontal or lateral moraines, or ice- polished rock surfaces.
    [Show full text]
  • 13. Late Pliocene-Pleistocene Glaciation
    13. LATE PLIOCENE - PLEISTOCENE GLACIATION W. A. Berggren, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts The discussion in this chapter is broken down into two increase in the former exceeding that of the latter; or parts: the first deals with glaciation in the North Atlantic as (v) less detritals, clay and carbonate deposited per unit time revealed in the data obtained on Leg 12; in the second part (that is, decreased sedimentation rate) with the decrease in an attempt is made to provide a chronologic framework of the latter exceeding the former. In view of the demon- Late Pliocene-Pleistocene glaciation and to correlate gla- strable increase in sedimentation rate above the preglacial/ cial/interglacial sequences as recorded in land and deep-sea glacial boundary at Sites 111, 112 and 116 due to increased sediments. amounts of detrital minerals and the fact that glacial periods in high latitudes are characterized by a carbonate GLACIATION IN THE NORTH ATLANTIC minimum (Mclntyre et al., in press) it can be seen that the One of the most significant aspects of Leg 12 was the correct explanation for the increase in natural gamma activ- various results which were obtained regarding glaciation in ity in the glacial part of the section is rather complex. Thin the North Atlantic. Glacial sediments were encountered at bands of carbonate were found at various levels intercalated all sites in the North Atlantic with the exception of Site with detrital-rich clays which indicates interglacial intervals, 117 (for the purpose of this discussion the North Atlantic so that the correct explanation probably lies with (iii) encompasses Sites 111 through 117; Sites 118 and 119 are above.
    [Show full text]
  • An Outline of the Quaternary Stratigraphy of Austria
    Quaternary Science Journal GEOzOn SCiEnCE MEDiA Volume 60 / number 2–3 / 2011 / 366–387 / DOi 10.3285/eg.60.2-3.09 iSSn 0424-7116 E&G www.quaternary-science.net An outline of the Quaternary stratigraphy of Austria Dirk van Husen, Jürgen M. Reitner Abstract: An overview of the Quaternary Stratigraphy in Austria is given. The subdivision of the mappable depositional units is based partly on criteria of lithostratigraphy (lithic properties) and allostratigraphy (e.g. unconformities). Traces of glaciations are missing for the Early Pleistocene period (2.58–0.78 Ma). The few and isolated sediment bodies are documenting fluvial accumulation and loess deposition along the rivers. Paleomagnetically correlated loess-paleosol-sequences like the profil at Stranzendorf including the Gauss/Matuyama boundary respectively Neogen/Quaternary are documenting slightly warmer condition than during during the Middle Pleistocene (0.78–0.13 Ma) which is in accordance with the global 18δ O record. Four major glaciations (Günz, Mindel, Riß, Würm) are proved during Middle and Late Pleistocene. All of these are documented by proglacial sediments topped by basal till, terminal moraines linked with terrace bodies and loess accumulation as well. This allows to recognize the climatic steering of sedimentation in context with advancing glaciers and the dispersion of permafrost and congelifraction as far as into the Alpine foreland. Both youngest major glaciations (Riß and Würm) are correlated according to geochronological data with the Marine Isotope Stages (MIS) 6 and 2. The simultaneousness of Günz and Mindel with the phases of massive global climatic deterioration during MIS 16 and 12 seems plausible.
    [Show full text]
  • The Classical European Glacial Stages: Correlation with Deep-Sea Sediments
    View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by UNL | Libraries University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Transactions of the Nebraska Academy of Sciences and Affiliated Societies Nebraska Academy of Sciences 1978 The Classical European Glacial Stages: Correlation with Deep-Sea Sediments George Kukla Columbia University Follow this and additional works at: https://digitalcommons.unl.edu/tnas Part of the Life Sciences Commons Kukla, George, "The Classical European Glacial Stages: Correlation with Deep-Sea Sediments" (1978). Transactions of the Nebraska Academy of Sciences and Affiliated Societies. 334. https://digitalcommons.unl.edu/tnas/334 This Article is brought to you for free and open access by the Nebraska Academy of Sciences at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Transactions of the Nebraska Academy of Sciences and Affiliated Societiesy b an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Transactions of the Nebraska Academy of Sciences- Volume VI, 1978 THE CLASSICAL EUROPEAN GLACIAL STAGES: CORRELATION WITH DEEP-SEA SEDIMENTS GEORGE KUKLA Lamont-Doherty Geological Observatory Of Columbia University Palisades, New York 10964 Four glacials and three interglacials, recognized by classical sea record revealed that this is not the case. In order to learn Alpine and North-European subdivisions of the Pleistocene, were cor­ the reasons for the discrepancy, we identified the type units related with continuous oxygen-isotope records from the oceans using and their boundaries at the type localities, correlated them loess sections and terraces as a link (Fig. 15). It was found that the Alpine "glacial" stages are represented by sediments formed during with the standard stratigraphic system, and tried to recognize both glacial and interglacial climates, that the classical Alpine "inter­ their true climatic characteristics.
    [Show full text]
  • LEVERETT the Amhurstburg Quadrangle but Are Very Scanty Further South
    Open File Report LXI The east border of Lake Rouge is marked by sandy deposits southward from the delta to about 2 miles into FIELD NOTES OF FRANK LEVERETT the Amhurstburg quadrangle but are very scanty further south. There is a very level tract with clay soil and Notebook No. 299 - Leverett scattered boulders over the area below the 600 contour as well as above it. COUNTY There is a slight suggestion of shore work west of Branch Lukerville, 1/8 mile ± from the crossroads with a Chippewa perceptible downward slope to the west and a slight Hillsdale sandy coating. This seems likely to mark the Lake Jackson Rouge limit. The shore is not clearly defined south or Keweenaw southwest from there so it is not feasible to trace it into Keweenaw Peninsula the head of the Big Creek drainage in the way I had Macomb hoped to do. The lake may have extended to within two Mackinac miles of the place where Big Creek is crossed by the Midland & Isabella M.C.R.R. east of the quarries. The valley of Big Creek is Monroe very narrow and sinuous for a mile above the railroad St. Clair bridge but is wider where the creek turns from a N.W. to Washtenaw a S.W. course. There is a wider channel on a small Wayne tributary north from there than on the creek above this OTHER STATES bend. It suggests a spillway coming in from the north. This seems to open out into a feature less plain within a Illinois mile from the bend of Big Creek.
    [Show full text]
  • European and Northwest African Middle Pleistocene Hominids1
    European and Northwest African Middle Pleistocene Hominids1 by F. Clark Howell THE SPARSE REPRESENTATION of human skeletal remains known from the Middle Pleistocene of Europe or from the Middle Pleistocene has always been one of the Africa with in situ human skeletal remains, stone im· greatest gaps in human-paleontological knowledge. At plements, and the bones of slaughtered animals. first, Southeastern Asia was unique in having provided These human skeletal remains, taken in conjunction remains from the Trinil beds in Java, but the signifi­ with those from the Middle Pleistocene of eastern and cance of this poorly preserved skull-cap was confirmed southern Asia, have an important bearing on interpre­ and greatly amplified by subsequent discoveries (Von tations of the course of human evolution. The signifi­ Koenigswald 1940) of better preserved specimens at cance of these discoveries has been obscured by the pre­ other localities of similar age, as well as in the still occupation of some human paleontologists with other older Djetis beds. Still tfuly unique in all the world is human remains either suspected to be of Pleistocene the somewhat younger occupation site of Locality 1 antiquity or questionable due to an extraordinary com· Choukoutien, with its extraordinarily abundant, prob­ plex of morphological features (the famous hoax of ably cannibalized, human remains in association with Piltdown). Largely as a consequence of this, there have hearths, stone implements (Choukoutienian chopper/ grown up two main interpretations of man's phylogeny chopping-tool complex), and remains of slaughtered in the Pleistocene, one depending on the possible im­ animals. portance of the suspicious "fossils," and the other de­ For many years, the only such find from the West was pending only on the scanty, but well-dated, human fos­ the enigmatic human mandible from the Grafenrain sils enumerated above.
    [Show full text]
  • Research History on the Tatra Mountains Glaciations
    S T U D I A G E O M O R P H O L O G I C A C A R P A T H O - B A L C A N I C A Vol. LI/LII, 2017/2018: 43–85 PL ISSN 0081-6434 PIOTR KŁAPYTA 1, JERZY ZASADNI 2 (KRAKÓW) RESEARCH HISTORY ON THE TATRA MOUNTAINS GLACIATIONS Abstract. In this paper, we provide a brief history of glacial geomorphologic research in the Tatra Mountains with a special focus on glacial chronologies. We provide critical comments on previously published glacial chronologies and identify relevant gaps in knowledge on Tatra mountain glacia- tions suggesting future challenges and the focus of scientific research. Distinct differences in applied methodologies, presented conceptions, and research paradigms over 160 years of research enable us to distinguish four phases of scientific research on Tatra mountain glaciation (pioneer phase, mapping phase, geochronological phase and meta-analysis phase). These four phases follow the universal sequence of glacial geomorphologic research history defined by P.D. Hughes et al. (2006) and P.D. Hughes and J.C. Woodward (2016) for Mediterranean mountain areas. In the last two phases, the glacial chronology was substantially supported with radiometric dating of landforms and sediments as well as paleobotanical data obtained from intra-moraine sites. The current me- ta-analysis phase of research provides dating techniques using terrestrial cosmogenic nuclide (TCN) exposure ages and glacier-climate modeling. The present-day TCN dataset for the Tatra Mountains includes 300 individual ages (10Be and 36Cl together). We underscore the fact that this dataset has substantially verified many key issues in the glacier geochronology of the Tatra Mountains.
    [Show full text]
  • The Plio-Pleistocene Glaciation in Eastern Europe, Siberia, and the Caucasus : Evolution of Thoughts
    The Plio-Pleistocene glaciation in eastern Europe, Siberia, and the Caucasus : evolution of thoughts Autor(en): Milanovsky, Evgeni E. Objekttyp: Article Zeitschrift: Eclogae Geologicae Helvetiae Band (Jahr): 93 (2000) Heft 3 PDF erstellt am: 05.10.2021 Persistenter Link: http://doi.org/10.5169/seals-168829 Nutzungsbedingungen Die ETH-Bibliothek ist Anbieterin der digitalisierten Zeitschriften. Sie besitzt keine Urheberrechte an den Inhalten der Zeitschriften. Die Rechte liegen in der Regel bei den Herausgebern. Die auf der Plattform e-periodica veröffentlichten Dokumente stehen für nicht-kommerzielle Zwecke in Lehre und Forschung sowie für die private Nutzung frei zur Verfügung. Einzelne Dateien oder Ausdrucke aus diesem Angebot können zusammen mit diesen Nutzungsbedingungen und den korrekten Herkunftsbezeichnungen weitergegeben werden. Das Veröffentlichen von Bildern in Print- und Online-Publikationen ist nur mit vorheriger Genehmigung der Rechteinhaber erlaubt. Die systematische Speicherung von Teilen des elektronischen Angebots auf anderen Servern bedarf ebenfalls des schriftlichen Einverständnisses der Rechteinhaber. Haftungsausschluss Alle Angaben erfolgen ohne Gewähr für Vollständigkeit oder Richtigkeit. Es wird keine Haftung übernommen für Schäden durch die Verwendung von Informationen aus diesem Online-Angebot oder durch das Fehlen von Informationen. Dies gilt auch für Inhalte Dritter, die über dieses Angebot zugänglich sind. Ein Dienst der ETH-Bibliothek ETH Zürich, Rämistrasse 101, 8092 Zürich, Schweiz, www.library.ethz.ch http://www.e-periodica.ch 0012-9402/00/030379-16 $1.50 + 0.20/0 Eclogae geol. Helv. 93 (2000) 379-394 Birkhäuser Verlag. Basel. 2000 The Plio-Pleistocene glaciation in eastern Europe, Siberia, and the Caucasus: Evolution of thoughts (Paper presented at the meeting of the International Commission on the Historv of Geological Sciences (1NHIGEO), Neuchâtel, Sept.
    [Show full text]
  • Human Evolution
    EDITORIAL BOARD EDITOR Alan Bryan COVER ARTWORK Bonnie Koenig SUBSCRIPTION EDITOR Linda Suss ASSOCIATE EDITORS KENELM BURRIDGE Department of Anthropology and Sociology, University of British Columbia, Vancouver, B.C. V6T 1W5 STEPHEN L. CUMBAA National Museum of Natural Sciences, 491 Bank St., Ottawa, Ontario K1A OM8 DELL HYMES Graduate School of Education, University of Pennsylvania, Philadelphia, Penn. 19104 JUNJI KOIZUMI Faculty of Arts, Aichi Kenritsu University, Nagoya 467 Japan RAY LeBLANC Archaeological Survey of Alberta, 8820 - 112 St., Edmonton, Alberta T6G 2P8 GERTRUDE NICKS Provincial Museum of Alberta, 12845 - 102 Ave., Edmonton, Alberta T5N OM6 TOM SHAY Department of Anthropology, University of Manitoba, Winnipeg, Man. T3T 2M6 The CANADIAN JOURNAL OF ANTHROPOLOGY/REVUE CANADIENNE D'ANTHRO- POLOGIE is published twice yearly (spring and fall) by the Department of Anthropology at the University of Alberta. MANUSCRIPTS These should be addressed to the Editor, CJA/RCA, Department of Anthropology, University of Alberta, Edmonton, Alberta, Canada, T6G 2H4. Instructions for the preparation of manuscripts can be found on the inside back cover. REPRINTS Fifty (50) reprints will be provided gratis to each author or group of authors. Additional reprints will be available at a cost to be determined. SUBSCRIPTIONS Please make cheques payable to: Canadian Journal of Anthropology. (Canadian Funds in Canada; U.S. Funds for all other countries) Individual: $15 per volume Institutional: $30 per volume Complete back file sets are available for continuing subscribers. Prices of back volumes and individ- ual issues available on request. ADVERTISEMENTS Information can be obtained by writing to The Editor. 0 1980 The Canadian Journal of Anthropology Revue Canadienne d'Anthropologie RICHARD FRUCHT MEMORIAL ESSAY PRIZE The CJA/RCA will award an annual prize in memory of Professor Richard Frucht for an essay on the general topic of historical materialism.
    [Show full text]
  • Abstract Volume 17Th Swiss Geoscience Meeting Fribourg, 22Nd + 23Rd November 2019
    Abstract Volume 17th Swiss Geoscience Meeting Fribourg, 22nd + 23rd November 2019 Geoscience goes underground: understanding resources & processes II Geoscience goes underground Knowledge of the shallow and deep underground has ever-growing importance in modern society. This is espe- cially true for Switzerland, which has a longstanding tradition of exploring the deep that was acquired over the course of decades of building tunnels throughout its territories. Hydrocarbon exploration of the Alpine Molasse Basin and the Jura fold-and-thrust belt yielded modest successes, but the public controversy regarding shale gas exploration and induced seismicity in the wake of deep geothermal exploration has highlighted the importance and the role of communication of our geoscientific knowledge to the public. The extraction of geothermal energy, building management, and land use planning will increasingly rely on knowledge of the near and deep subsurface geology. Natural resources of the underground, such as geothermal energy (from shallow to deep), CO2 sequestration, shale gas, reservoir technology, water exploitation, subsurface energy storage, or “classic” mineral resources will thereby play a central role in the future. Geodata, GeoBIM, GeoCIM projects, and 3D geology models will reshape future management and use of underground resources and geoscientists must not miss the opportunity to get involved. Indeed, geoscientists should reach out to poli- ticians and the public and take a position in a debate that will become increasingly more complex.
    [Show full text]
  • The Late Neogene-Quaternary Tectonic Mobility of the Polish West Carpathians a Case Study of the Dunajec Drainage Basin (Pi
    ANNALES SOCIETATIS GEOLOGORUM POLONIAE ROCZNIK POLSKIEGO TOWARZYSTWA GEOLOGICZNEGO v. 54-1/2: 133-189 Kraków 1984 Witold Z u c h ie w ic z THE LATE NEOGENE-QUATERNARY TECTONIC MOBILITY OF THE POLISH WEST CARPATHIANS A CASE STUDY OF THE DUNAJEC DRAINAGE BASIN (PI. I - V , Figs. 1-14) Późnoneogeńsko-czwartorzędowa mobilność tektoniczna polskich Karpat Zachodnich na przykładzie dorzecza Dunajca (PI. I -V , Fig. 1-14) Witold Zuchiewicz: The Late Neogene-Quaternary tectonic mobility of the Polish West Carpathians. A case study of the Dunajec drainage basin. Ann. Soc. Geol. Poloniae 54-1/2:133-189, 1984. Kraków. Abstract: The article deals with neotectonic movements which have been affecting the Dunajec drainage basin since the Sarmatian. The amount and intensity of these movements have been calculated and compared with the geological structure of the basin. It seems probable that the Plio- -Pleistocene tectonics of the West Carpathians reflects tectonic mobility of the flysch substratum. This mobility may refer to the still continuing process of backward thrusting of the Easteuropean Platform under the Carpathians. K e y words: neotectonic movements, geomorphology, Neogene, Quaternary, Dunajec drainage basin, West Carpathians. Witold Zuchiewicz: Institute of Geological Sciences, Jagiellonian University, 2A Oleandry Str., 30-063, Kraków. manuscript received: April, 1981 accepted: October, 1982 Treść: Artykuł omawia ruchy neotektoniczne zachodzące w obrębie dorzecza Dunajca (polskie Karpaty Zachodnie), począwszy od sarmatu. Obliczone rozmiary i prędkości tych ruchów przeanalizo­ wano na tle budowy geologicznej dorzecza. Piioceńsko-czwartorzędowa aktywność tektoniczna Karpat Zachodnich może odzwierciedlać mobilność podłoża fliszu, związaną z niezakończonym jeszcze pro­ cesem podsuwania się podłoża platformowego pod Karpaty.
    [Show full text]
  • Correlation Between the Quaternary Continental Sediments in Nortl:L-Eastern Bulgarra with the Marine Sediments in the Black Sea Shelf
    GEOLOGICA BALC\NICA, 24. 5, Sofia, Oct. 1994, p . 3-10 Correlation between the Quaternary continental sediments in Nortl:l-eastern Bulgarra with the marine sediments in the Black Sea Shelf V. Shopov, J. Evlogiev, N. Popov Geological Institute, Bulg. Acad. Sci. 111 3 Sofia (Received 26. 01. 1994; accepted 24 . 03. 1994) I 8 , monoo, fl. Eo;IO~IIe6, H. flonoo - KoppeARI{Ufl Me:I'Cay 'lemoepmU'IHblMU KOHI/lUHeHmaAbHblMU Ofn J!O:JICe­ HUflMU Ceoepo-BocmO'IHOiJ. 5oA•apuu u AtopcKUMu omArxHr:eHURMU IJepHOMopcKOi!O meAbr/Ja. Cesepo-BecTo'IHaH EioJJrapHH 6bl,13 3KCTpar JI!IUHaJibHOH o6JJaCTbiO B Te'leHHe 'leTBePTH'IHOTO nepHO)la. AKTHBHaH 3p03HH H a6pa3HR 3JJ.ecb C'IHTaercH cBH3auuoii c nJJIOBHaJJbHblMH !j>a3aMH JieJJ.HHKOBbiBbiX 3nox. AJIJJIOBHaJibHbie orno­ >KeHHR reppac T 0- T 6, uaKonHBWHecH npH cooTBeTCTBYIOli\HX rnHUHaJJbHblX H cTaJJ.llaJibHbiX UHKJJax, 6blJJH nepBOHCTO'IHHKOM JiecCOBOfO MeJJK03eMa. JlecCOBbiH aKKyMyJIHT, o6pa30BaBWHikR npH J).aHHOM UHKJie, 3aJJe­ raeT Ha OOJJee JJ.peBHHX Tepapcax H CTyneHRX, KOTOpble 6biJIH OTKpbiTbl Jl.JJR 30JIOBOH CeJJ.HMeHTaUHH . AKTHB· HYIO 30JIOBYIO JJ.eHTeJJbHOCTb HY>KHO cBH3aTb c !j>a3aMH .n.erJIHUHaUHH JJeJJ.HHKOB . B 4epuoMopcKoii o6.nacTH OTMe'leHbl 3<1><!>eKTbl nHTH 60JJbWHX OJJeJJ.eHeHHH, COOTBeTCTBYIOlllHX perpecCHHM MOpR, C Ha'laJJa 'leTsepTH'I· HOro nepHOJJ.a: JJ.YHBBHH, f10Hll3, MHHJJ.eJJH, pHCa H B!OpMa. AJJJJIOBH3JJbHaSJ flO'IBa Ha.ll. Ce.ll.bMbJM JJeCCOM CBH· )leTeJJbcTByeT, 'ITO B 3TO speMH npoH3oweJI nepepbiR s ceJJ.HMeHTaUHH - perpeccHll fiOHUa-2. AJJJIIOBHH ua.n. wecTbiM JieCCOM COOTBeTCTByeT MHH.ll.MbCKOH perpeCHH, Ha.ll. flHTbiM JieCCOM - perpecCHH pHCa-1, a HaJJ. 'leTBepTbiM JleCCOM, MO>KeT 6b1Tb, COOTBeTByeT perpecCHH pHca-2.
    [Show full text]