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Programme Monday, March 24
23rd LAK, 2014, Heidelberg Programme 13 Programme Monday, March 24 INF 252, Hörsäle Chemie 18:00– CONFERENCE DESK OPENING 21:00 18:00– ICEBREAKER PARTY 22:00 * Sponsored by DFG travel grants 14 Programme 23rd LAK, 2014, Heidelberg Tuesday I, March 25 INF 252, Hörsaal Ost INF 252, Hörsaal West 09:30 Welcome Christina Ifrim and Wolfgang Stinnesbeck DAAD-Fördermöglichkeiten für Geowissenschaftler aus/nach Lateinamerika Sybilla Tinnap, DAAD, Bonn Talk 141: Funding Opportunities for Scientific and Technological Cooperation: The Role of the Project Management Agency European and International Cooperation International Bureau of the Bmbf Inge Lamberz de Bayas, Internationales Büro, Bundesministerium für Bildung und Forschung, Bonn International Cooperation in DFG-Programmes – Earth Sciences in Latin America Dietrich Halm, DFG, Bonn 11:00 COFFEE BREAK and POSTER SESSION Session 1: The southernmost dinosurs in Latin Session 2: Water America and their environment Chair: Heinrich Adolf Horn Chair: Marcelo Leppe 11:20 Talk 205: Late Cretaceous Terrestrial Biota from Las Talk 132: Nutrient fluxes in the groundwater affecting Chinas-Cerro Guido Complex, Magallanes Region, the northern mangrove coast of the peninsula Yucatán Southern Chile: A Key Area for the Antarctic-South (México) American Biogeography Lisa Krienen, Thomas Rüde, Eduardo Graniel Castro and Antonio Marcelo Leppe, Wolfgang Stinnesbeck, Eberhard Frey, Héctor Cardona Benavides Mansilla, Manfred Vogt, Edwin Gonzalez, Leslie Manriquez, Katherine Cisternas, Maritza Mihoc and Toshiro Jujihara -
FAD. See First Appearance Datum Fagaloa Trend, 330759 Faial, 33, 820505 Faial Island, Basalt, Alkali, 820453, 820454, 820455
346 FAD F Africa W, 360043, 360101, 361003 glauconite, authigenic, 710361 FAD. See first appearance datum alteration, 711003 gypsum, authigenic, 710361 Fagaloa trend, 330759 Angola Basin, evolution, geologic, 750530 heat flow, 710299, 710302 Faial, 33, 820505 anoxia, global, evidence against, 801003 thermal conductivity, 710300 Faial Island, basalt, alkali, 820453, 820454, Antarctica, 361051 humic acid, 711048 820455 geochemistry, 711011 chemistry, 711045 fairchildite, clay minerals, hydrothermal aromatic fraction, 711008 kerogen, 711048, 711049 mounds, 700225 Atlantic Ocean, Cretaceous, 750820 organic matter, 711045 Fairway Ridge, 901339 Atlantic Ocean S shale, black, 711049 Lansdowne Bank, Neogene sequence, 901339 Cretaceous, 720981, 720982 humic compounds, 711006 Faisi, 160663 hiatuses, 391099, 391101, 391104 carbon, organic, 711006 Falcon E, 040592 Mesozoic, 751035, 751040, 751041 mudstone, black, 711006 Falcon Formations, 040597 Atlantic Ocean SW poor yield, 711006 Falconara, Sicily, 42A0777 basin, evolution, 360993, 360994, 360996, hydrocarbon, 711033 Falkland Escarpment, 360966, 710021, 710285 360998, 360999, 361000, 361001, 361002, carbon, organic, 711033 Falkland Fracture Zone, 360008, 360027, 361004, 361005, 361006, 361007, 361008, hydrocarbon, C,-C7, 711033 360100, 360101, 360259, 360494, 360538, 361009 hydrocarbon, light, 711033 360962, 361004, 710302, 710470, 710830, paleoenvironment, 710320, 710321, 710328 kerogen, 711033 720017, 730791, 750479 sediments, 711001 low molecular weight, 711033, 711034 Atlantic Ocean S authigenic -
New Detrital Zircon U/Pb Geochronology of the Cerro Dorotea, Río Turbio, and Río Guillermo Formations, Magallanes Basin
O EOL GIC G A D D A E D C E I H C I L E O S F u n 2 d 6 la serena octubre 2015 ada en 19 Timing and rates of foreland sedimentation: New detrital zircon U/Pb geochronology of the Cerro Dorotea, Río Turbio, and Río Guillermo formations, Magallanes basin Julie C. Fosdick1*, J. Enrique Bostelmann2, Joel Leonard1, Raúl Ugalde3, José Luis Oyarzún4, and Miguel Griffin5 1: Department of Geological Sciences, Indiana University, 1001 Tenth Street, Bloomington, Indiana, 47405, USA. 2: Red Paleontológica U-Chile, Laboratorio de Ontogenia y Filogenia, Departamento de Biología, Facultad de Ciencias, Universidad de Chile, Santiago, Chile. 3: PEDECIBA Geociencias, Facultad de Ciencias, Universidad de la República, Iguá 4225, Montevideo, Uruguay. 4: Parque Geo-paleontológico La Cumbre-Baguales, Ruta 9 km 284, Magallanes, Chile. 5: CONICET—División PaleoZoología Invertebrados, Museo de La Plata. Paseo del Bosque s/n, La Plata, Argentina. * email: [email protected] Abstract. We report new detrital zircon U/Pb signals (timing, tempo, magnitude) of tectonics, climate, geochronology from the Cenozoic Magallanes foreland and eustasy in the stratigraphic record. For instance, basin (near 51 °S) in both Argentina and Chile, that sheds enhanced tectonism in foreland basin settings can cause light on sedimentary provenance and improved timing of crustal load-driven subsidence and basin deepening. sedimentation for the Cerro Dorotea, Río Turbio, and Río Globally, the growth and ablation of continental ice sheets Guillermo formations. Using youngest detrital age regulates sea level and global climate, and precipitation populations to constrain maximum depositional age (MDA), and temperature gradients influence erosion rates, we provide the first radiometric age confirmation of vegetation cover, and the distribution of deformation. -
Geology and Oil Resources of the Western Puente Hills Area, Southern California
L: ... ARY Geology and Oil Resources of the Western Puente Hills Area, Southern California GEOLOGICAL SURVEY PROFESSIONAL PAPER 420-C Geology and Oil Resources of the Western Puente Hills Area, Southern California By R. F. YERKES GEOLOGY OF THE EASTERN LOS ANGELES BASIN, SOUTHERN CALifORNIA GEOLOGICAL SURVEY PROFESSIONAL PAPER 420-C A study of the stratigraphy, structure, and oil resources of the La Habra and Whittier quadrangles UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1972 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress catalog-card No. 72-600163 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Page Abstract __________________________________________ _ Structure _________________________________________ _ C1 c 28 Introduction ______________________________________ _ 2 Whittier fault zone _____________________________ _ 29 Location and purpose __________________________ _ 2 Workman Hill fault ____________________________ _ Previous work _________________________________ _ 29 3 Whittier Heights fault __________________________ _ 30 Methods and acknowledgments ________________ .,. __ 3 Rowland fault _________________________________ _ Stratigraphy ______________________________________ _ 31 4 Norwalk fault _________________________________ _ Rocks of the basement complex _________________ _ 4 31 Unnamed greenschist ________ . _______________ _ Historic ruptures _______________ -
California State University, Northridge the Geology Of
CALIFORNIA STATE UNIVERSITY, NORTHRIDGE THE GEOLOGY OF THE INNER BASIN MARGIN, NEWPORT BEACH TO DANA POINT, ORANGE COUNTY, CALIFORNIA A thesis submitted in partial satisfaction of the requirements for the degree of Master of Science in Geology by Stephen Charles Sterling January, 1982 The Thesis of Stephen Charles Sterling is approved: California State University, Northridge i i CONTENTS Page ABSTRACT INTRODUCTION 1 General Statement 1 Geographic Setting Bathymetric Setting 2 Previous Investigations 2 METHODS AND PROCEDURES 7 General Statement 7 Navigation 10 Velocity Analysis 10 Velocity Functions 11 Depth Migration 13 Ac know l edgemen ts 13 GEOLOGIC SETTING 15 REGIONAL STRATIGRAPHY 23 General Statement 23 Basement 23 Superjacent Rocks 26 Jurassic-Early Miocene 26 Middle to Late Miocene 27 Pliocene 32 Pleistocene 36 Holocene 37 SEISMIC STRATIGRAPHY 38 General Statement 38 iii Page Basement 38 r1i ocene 39 Pliocene 43 ONSHORE STRUCTURE 48 OFFSHORE STRUCTURE 52 General Statement 52 Faults 52 The Newport-Inglewood Fault Zone 52 Other Faults 58 Structural Highs and Lows 61 Correlation of Onshore-Offshore Geologic Features 63 NEOGENE EVOLUTION OF THE INNER BASIN MARGIN 67 General Statement 67 Pre-depositional Events 67 Neogene Events 69 Depositional History 69 Structural Evolution 73 SUMMARY AND CONCLUSIONS 75 REFERENCES 80 iv LIST OF ILLUSTRATIONS Figure Page .,.. l. Location of study area 4 2. Bathymetry of the inner basin margin 5 3. Tracklines of common depth point seismic lines in the study area 9 4. Major structural blocks of the Los Angeles basin 17 5. Location of geologic features referred to in text 19 6. Composite sections showing regional correlation of units 24 7. -
Paleontological Discoveries in the Chorrillo Formation (Upper Campanian-Lower Maastrichtian, Upper Cretaceous), Santa Cruz Province, Patagonia, Argentina
Rev. Mus. Argentino Cienc. Nat., n.s. 21(2): 217-293, 2019 ISSN 1514-5158 (impresa) ISSN 1853-0400 (en línea) Paleontological discoveries in the Chorrillo Formation (upper Campanian-lower Maastrichtian, Upper Cretaceous), Santa Cruz Province, Patagonia, Argentina Fernando. E. NOVAS1,2, Federico. L. AGNOLIN1,2,3, Sebastián ROZADILLA1,2, Alexis M. ARANCIAGA-ROLANDO1,2, Federico BRISSON-EGLI1,2, Matias J. MOTTA1,2, Mauricio CERRONI1,2, Martín D. EZCURRA2,5, Agustín G. MARTINELLI2,5, Julia S. D´ANGELO1,2, Gerardo ALVAREZ-HERRERA1, Adriel R. GENTIL1,2, Sergio BOGAN3, Nicolás R. CHIMENTO1,2, Jordi A. GARCÍA-MARSÀ1,2, Gastón LO COCO1,2, Sergio E. MIQUEL2,4, Fátima F. BRITO4, Ezequiel I. VERA2,6, 7, Valeria S. PEREZ LOINAZE2,6 , Mariela S. FERNÁNDEZ8 & Leonardo SALGADO2,9 1 Laboratorio de Anatomía Comparada y Evolución de los Vertebrados. Museo Argentino de Ciencias Naturales “Bernardino Rivadavia”, Avenida Ángel Gallardo 470, Buenos Aires C1405DJR, Argentina - fernovas@yahoo. com.ar. 2 Consejo Nacional de Investigaciones Científicas y Técnicas, Argentina. 3 Fundación de Historia Natural “Felix de Azara”, Universidad Maimonides, Hidalgo 775, C1405BDB Buenos Aires, Argentina. 4 Laboratorio de Malacología terrestre. División Invertebrados Museo Argentino de Ciencias Naturales “Bernardino Rivadavia”, Avenida Ángel Gallardo 470, Buenos Aires C1405DJR, Argentina. 5 Sección Paleontología de Vertebrados. Museo Argentino de Ciencias Naturales “Bernardino Rivadavia”, Avenida Ángel Gallardo 470, Buenos Aires C1405DJR, Argentina. 6 División Paleobotánica. Museo Argentino de Ciencias Naturales “Bernardino Rivadavia”, Avenida Ángel Gallardo 470, Buenos Aires C1405DJR, Argentina. 7 Área de Paleontología. Departamento de Geología, Universidad de Buenos Aires, Pabellón 2, Ciudad Universitaria (C1428EGA) Buenos Aires, Argentina. 8 Instituto de Investigaciones en Biodiversidad y Medioambiente (CONICET-INIBIOMA), Quintral 1250, 8400 San Carlos de Bariloche, Río Negro, Argentina. -
Importance of Predecessor Basin History on the Sedimentary Fill of A
EAGE Basin Research (2010) 22, 640–658, doi: 10.1111/j.1365-2117.2009.00443.x Importance of predecessor basin history on the sedimentary fill of a retroarc foreland basin: provenance analysis of the Cretaceous Magallanes basin, Chile (50^521S) B. W. Romans,n A. Fildani,w S. A. Graham,n S. M. Hubbardz and J. A. Covaultn nDepartment of Geological & Environmental Sciences, Stanford University, Stanford, CA, USA wChevron EnergyTechnology Company, Clastic Stratigraphy R&D, San Ramon, CA, USA zDepartment of Geoscience, University of Calgary,Calgary,AB, Canada ABSTRACT An integrated provenance analysis of the Upper Cretaceous Magallanes retroarc foreland basin of southern Chile (501300^521S) provides new constraints on source area evolution, regional patterns of sediment dispersal and depositional age. Over 450 new single-grain detrital-zircon U-Pb ages, which are integrated with sandstone petrographic and mudstone geochemical data, provide a comprehensive detrital record of the northern Magallanes foreland basin- ¢lling succession (44000- m-thick). Prominent peaks in detrital-zircon age distribution among the Punta Barrosa, CerroToro, TresPasos andDoroteaFormations indicate thatthe incorporation and exhumation ofUpperJurassic igneous rocks (ca.147^155Ma) into the Andean fold-thrust belt was established in the Santonian (ca. 85 Ma) andwas a signi¢cant source of detritus to the basin by the Maastrichtian (ca.70 Ma). Sandstone compositional trends indicate an increase in volcanic and volcaniclastic grains upward through the basin ¢ll corroborating the interpretation of an unroo¢ng sequence. Detrital-zircon ages indicate that the Magallanes foredeep received young arc-derived detritus throughout its ca. 20 m.y.¢lling history,constraining the timing of basin- ¢lling phases previously based only on biostratigraphy. -
Structural Evolution of the Northernmost Andes, Colombia
Structural Evolution of the Northernmost Andes, Colombia GEOLOGICAL SURVEY PROFESSIONAL PAPER 846 Prepared in coopeTation ·with the lnstituto Nacional de Investigaciones Geologico-MineTas under the auspices of the Government of Colombia and the Agency for International Development) United States DepaTtment of State Structural Evolution of the Northernmost Andes, Colombia By EARL M. IRVING GEOLOGICAL SURVEY PROFESSIONAL PAPER 846 Prepared in cooperation ·with the lnstituto Nacional de Investigaciones Geologico-Min eras under the auspices of the Government of Colombia and the Agency for International Development) United States Department of State An interpretation of the geologic history of a complex mountain system UNITED STATES GOVERNlVIENT PRINTING OFFICE, vVASHINGTON 1975 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress Cataloging in Publication Data Irving, Earl Montgomery, 1911- Structural evolution of the northernmost Andes, Columbia. (Geological Survey professional paper ; 846) Bibliography: p Includes index. Supt. of Docs. no.: I 19.16:846 1. Geology-Colombia. 2. Geosynclines----Colombia. I. Instituto Nacional de Investigaciones Geologico Mineras.. II. Title. III. Series: United States. Geological Survey. Professional paper ; 846. QE239.175 558.61 74-600149 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402- Price $1.30 (paper cover) Stock Number 2401-02553 CONTENTS Page Pasre Abstract ---------------------------------------- -
From the Late Cretaceous of the Magallanes Basin, Chilean Patagonia
Andean Geology ISSN: 0718-7092 [email protected] Servicio Nacional de Geología y Minería Chile Otero, Rodrigo A.; Soto-Acuña, Sergio; Salazar S., Christian; Oyarzún, José Luis New elasmosaurids (Sauropterygia, Plesiosauria) from the Late Cretaceous of the Magallanes Basin, Chilean Patagonia: Evidence of a faunal turnover during the Maastrichtian along the Weddellian Biogeographic Province Andean Geology, vol. 42, núm. 2, mayo, 2015, pp. 237-267 Servicio Nacional de Geología y Minería Santiago, Chile Available in: http://www.redalyc.org/articulo.oa?id=173938242005 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Andean Geology 42 (2): 237-267. May, 2015 Andean Geology doi: 10.5027/andgeoV42n1-a05 www.andeangeology.cl New elasmosaurids (Sauropterygia, Plesiosauria) from the Late Cretaceous of the Magallanes Basin, Chilean Patagonia: Evidence of a faunal turnover during the Maastrichtian along the Weddellian Biogeographic Province * Rodrigo A. Otero1, Sergio Soto-Acuña1, 2, Christian Salazar S.2, José Luis Oyarzún3 1 Red Paleontológica U-Chile, Laboratorio de Ontogenia y Filogenia, Departamento de Biología, Facultad de Ciencias, Universidad de Chile, Las Palmeras 3425, Santiago, Chile. [email protected], [email protected] 2 Área Paleontología, Museo Nacional de Historia Natural, Casilla 787, Santiago, Chile. [email protected] 3 Miraflores 863, Puerto Natales, Chile. [email protected] * Corresponding author: [email protected] ABSTRACT. Several Upper Cretaceous plesiosaur specimens recovered from southernmost Chile are described here. These were collected from upper levels of the Dorotea Formation exposed on three different localities (Sierra Baguales, Cerro Castillo, and Dumestre). -
Paleontological Resources Technical Report for the Villages at the Alhambra Project, Alhambra, Los
Paleontological Resources Technical Report for The Villages at The Alhambra Project, Alhambra, Los Angeles County, California April 2019 PREPARED FOR The Ratkovich Company 1000 S. Fremont Avenue, Unit 1 Building A1, Suite 1150 Alhambra, California 91803 PREPARED BY SWCA Environmental Consultants 51 West Dayton Street Pasadena, CA 91105 Paleontological Resources Technical Report For The Villages at The Alhambra Project, Alhambra, Los Angeles County, California Prepared for The Ratkovich Company 1000 S. Fremont Avenue, Unit 1 Building A1, Suite 1150 Alhambra, California 91803 Prepared by Alyssa Bell, Ph.D. SWCA Environmental Consultants 51 West Dayton Street Pasadena, CA 91105 (626) 240-0587 www.swca.com SWCA Project No. 49511 April 2019 Paleontological Resources Technical Report for The Villages at Alhambra Project, Alhambra, Los Angeles County, California EXECUTIVE SUMMARY Purpose and Scope: The Ratkovich Company retained SWCA Environmental Consultants (SWCA) to conduct a paleontological resources study in support of the proposed The Villages at The Alhambra Project (project) located in the city of Alhambra, Los Angeles County, California. This paleontological resources study is intended to characterize and describe paleontological resources identified within the project area that could be affected by ground-disturbing activities associated with the project. The Ratkovich Company proposes to develop an urban neighborhood across the project site, including a network of landscape and communal spaces that fuse office and residential uses into a single community with a unique identity and sense of place. Active uses will be featured along street frontages to avoid blank walls and visible parking areas. All but one of the existing office buildings on the site would be retained as part of the project. -
Geologic Resources Inventory Ancillary Map Information Document for Santa Monica Mountains National Recreation Area
U.S. Department of the Interior National Park Service Natural Resource Stewardship and Science Directorate Geologic Resources Division Santa Monica Mountains National Recreation Area GRI Ancillary Map Information Document Produced to accompany the Geologic Resources Inventory (GRI) Digital Geologic Data for Santa Monica Mountains National Recreation Area samo_geology.pdf Version: 8/4/2016 I Santa Monica Mountains National Recreation Area Geologic Resources Inventory Ancillary Map Information Document for Santa Monica Mountains National Recreation Area Table of Contents Geolog.i.c. .R...e..s.o..u..r.c..e..s.. .I.n..v.e..n..t.o..r..y. .M...a..p.. .D..o..c..u..m...e..n..t....................................................................... 1 About th..e.. .N...P..S.. .G...e..o..l.o..g..i.c. .R...e..s.o..u..r.c..e..s.. .I.n..v.e..n..t.o..r..y. .P...r.o..g..r.a..m........................................................... 3 GRI Dig.i.t.a..l. .M...a..p..s. .a..n..d.. .S...o..u..r.c..e.. .M..a..p.. .C...i.t.a..t.i.o..n..s........................................................................... 5 Digital G...e..o..l.o..g..i.c.. .M..a..p.. .o..f. .S...a..n..t.a.. .M..o..n..i.c..a.. .M...o..u..n..t.a..i.n..s. .N...a..t.i.o..n..a..l. .R..e..c..r.e..a..t.i.o..n.. .A..r.e..a.......................... 6 Map Un..it. .L..i.s..t................................................................................................................................................................. 6 Map Un..it. .D...e..s..c..r.i.p..t.io..n..s................................................................................................................................................... -
Geology of Southeastern Ventura Basin Los Angeles County California
Geology of Southeastern Ventura Basin Los Angeles County California By E. L. WINTERER and D. L. DURHAM SHORTER CONTRIBUTIONS TO GENERAL GEOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 334-H A study of the stratigraphy, structure, and occurrence of oil in the late Cenozoic Ventura basin UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1962 UNITED STATES DEPARTMENT OF THE INTERIOR STEW ART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, D.C. CONTENTS Page Page Abstract ____________________________________________ 275 Stratigraphy Continued Introduction.______________________________________ 276 Tertiary system Continued Purpose and scope.------_______________________ 276 Pliocene series..._________------__---__----- 308 Fieldwork __ __________________________________ 276 Pico formation.____________-_----_-_-_- 308 Acknowledgments. _ _----_-_-.________________- 276 Stratigraphy and lithology___________ 309 Geography. _________________________________________ 278 Newhall-Potrero area__________ 309 Climate- ______--_-__-_-__-_--_-_____________-_ 278 Newhsll-Potrero oil field to East Vegetation.____________________________________ 278 Canyon____________________ 310 Santa Clara River______________________________ 278 Mouth of East Canyon to San Fer Relief. __.._.._._._________---_-_--_________ 278 nando Pass__-----_-_-------- 311 Human activities----_------__--________________ 278 San Fernando Pass to San Gabriel Physiography_ _____________________________________ 278 fault..____-__-__-_------.--_ 311 Structural and lithologic control of drainage______ 279 Santa Clara River to Del Valle River terraces and old erosion surfaces-__ _________ 279 fault.___----.--_-_---------_ 312 Present erosion cycle.___________________________ 281 Del Valle fault to Holser fault__ 312 Landslides- ___--.-------_-_--___________________ 281 Area north of Holser fault- ______ 312 Stratigraphy.______________________________________ 281 Fossils..