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Apatite Thermochronology in Modern Geology
Downloaded from http://sp.lyellcollection.org/ by guest on September 24, 2021 Apatite thermochronology in modern geology F. LISKER1*, B. VENTURA1 & U. A. GLASMACHER2 1Fachbereich Geowissenschaften, Universita¨t Bremen, PF 330440, 28334 Bremen, Germany 2Institut fu¨r Geowissenschaften, Ruprecht-Karls-Universita¨t Heidelberg, Im Neuenheimer Feld 234, 69120 Heidelberg, Germany *Corresponding author (e-mail: fl[email protected]) Abstract: Fission-track and (U–Th–Sm)/He thermochronology on apatites are radiometric dating methods that refer to thermal histories of rocks within the temperature range of 408–125 8C. Their introduction into geological research contributed to the development of new concepts to interpreting time-temperature constraints and substantially improved the understanding of cooling processes within the uppermost crust. Present geological applications of apatite thermochronological methods include absolute dating of rocks and tectonic processes, investigation of denudation histories and long-term landscape evolution of various geological settings, and basin analysis. Thermochronology may be described as the the analysis of radiation damage trails (‘fission quantitative study of the thermal histories of rocks tracks’) in uranium-bearing, non-conductive using temperature-sensitive radiometric dating minerals and glasses. It is routinely applied on the methods such as 40Ar/39Ar and K–Ar, fission minerals apatite, zircon and titanite. Fission tracks track, and (U–Th)/He (Berger & York 1981). are produced continuously through geological time Amongst these different methods, apatite fission as a result of the spontaneous fission of 238U track (AFT) and apatite (U–Th–Sm)/He (AHe) atoms. They are submicroscopic features with an are now, perhaps, the most widely used thermo- initial width of approximately 10 nm and a length chronometers as they are the most sensitive to low of up to 20 mm (Paul & Fitzgerald 1992) that can temperatures (typically between 40 and c. -
Carnivora from the Late Miocene Love Bone Bed of Florida
Bull. Fla. Mus. Nat. Hist. (2005) 45(4): 413-434 413 CARNIVORA FROM THE LATE MIOCENE LOVE BONE BED OF FLORIDA Jon A. Baskin1 Eleven genera and twelve species of Carnivora are known from the late Miocene Love Bone Bed Local Fauna, Alachua County, Florida. Taxa from there described in detail for the first time include the canid cf. Urocyon sp., the hemicyonine ursid cf. Plithocyon sp., and the mustelids Leptarctus webbi n. sp., Hoplictis sp., and ?Sthenictis near ?S. lacota. Postcrania of the nimravid Barbourofelis indicate that it had a subdigitigrade posture and most likely stalked and ambushed its prey in dense cover. The postcranial morphology of Nimravides (Felidae) is most similar to the jaguar, Panthera onca. The carnivorans strongly support a latest Clarendonian age assignment for the Love Bone Bed. Although the Love Bone Bed local fauna does show some evidence of endemism at the species level, it demonstrates that by the late Clarendonian, Florida had become part of the Clarendonian chronofauna of the midcontinent, in contrast to the higher endemism present in the early Miocene and in the later Miocene and Pliocene of Florida. Key Words: Carnivora; Miocene; Clarendonian; Florida; Love Bone Bed; Leptarctus webbi n. sp. INTRODUCTION can Museum of Natural History, New York; F:AM, Frick The Love Bone Bed Local Fauna, Alachua County, fossil mammal collection, part of the AMNH; UF, Florida Florida, has produced the largest and most diverse late Museum of Natural History, University of Florida. Miocene vertebrate fauna known from eastern North All measurements are in millimeters. The follow- America, including 43 species of mammals (Webb et al. -
71St Annual Meeting Society of Vertebrate Paleontology Paris Las Vegas Las Vegas, Nevada, USA November 2 – 5, 2011 SESSION CONCURRENT SESSION CONCURRENT
ISSN 1937-2809 online Journal of Supplement to the November 2011 Vertebrate Paleontology Vertebrate Society of Vertebrate Paleontology Society of Vertebrate 71st Annual Meeting Paleontology Society of Vertebrate Las Vegas Paris Nevada, USA Las Vegas, November 2 – 5, 2011 Program and Abstracts Society of Vertebrate Paleontology 71st Annual Meeting Program and Abstracts COMMITTEE MEETING ROOM POSTER SESSION/ CONCURRENT CONCURRENT SESSION EXHIBITS SESSION COMMITTEE MEETING ROOMS AUCTION EVENT REGISTRATION, CONCURRENT MERCHANDISE SESSION LOUNGE, EDUCATION & OUTREACH SPEAKER READY COMMITTEE MEETING POSTER SESSION ROOM ROOM SOCIETY OF VERTEBRATE PALEONTOLOGY ABSTRACTS OF PAPERS SEVENTY-FIRST ANNUAL MEETING PARIS LAS VEGAS HOTEL LAS VEGAS, NV, USA NOVEMBER 2–5, 2011 HOST COMMITTEE Stephen Rowland, Co-Chair; Aubrey Bonde, Co-Chair; Joshua Bonde; David Elliott; Lee Hall; Jerry Harris; Andrew Milner; Eric Roberts EXECUTIVE COMMITTEE Philip Currie, President; Blaire Van Valkenburgh, Past President; Catherine Forster, Vice President; Christopher Bell, Secretary; Ted Vlamis, Treasurer; Julia Clarke, Member at Large; Kristina Curry Rogers, Member at Large; Lars Werdelin, Member at Large SYMPOSIUM CONVENORS Roger B.J. Benson, Richard J. Butler, Nadia B. Fröbisch, Hans C.E. Larsson, Mark A. Loewen, Philip D. Mannion, Jim I. Mead, Eric M. Roberts, Scott D. Sampson, Eric D. Scott, Kathleen Springer PROGRAM COMMITTEE Jonathan Bloch, Co-Chair; Anjali Goswami, Co-Chair; Jason Anderson; Paul Barrett; Brian Beatty; Kerin Claeson; Kristina Curry Rogers; Ted Daeschler; David Evans; David Fox; Nadia B. Fröbisch; Christian Kammerer; Johannes Müller; Emily Rayfield; William Sanders; Bruce Shockey; Mary Silcox; Michelle Stocker; Rebecca Terry November 2011—PROGRAM AND ABSTRACTS 1 Members and Friends of the Society of Vertebrate Paleontology, The Host Committee cordially welcomes you to the 71st Annual Meeting of the Society of Vertebrate Paleontology in Las Vegas. -
Structure and Evolution of the Petroliferous Euphrates Graben System, Southeast Syria1
Structure and Evolution of the Petroliferous Euphrates Graben System, Southeast Syria1 Robert K. Litak,2 Muawia Barazangi,3 Graham Brew,3 Tarif Sawaf,4 Anwar Al-Imam,4 and Wasif Al-Youssef4 ABSTRACT Cenozoic inversion of some structures also is evi- dent. Approximately 30 oil fields have been dis- The northwest-trending Euphrates graben sys- covered in the Euphrates graben system since tem is an aborted intracontinental rift of Late 1984. Recoverable reserves discovered to date Cretaceous age that has subsequently been hidden reportedly exceed 1 billion barrels of oil and less- by Cenozoic burial. Approximately 100 km wide, er amounts of gas. Light oil is primarily found in the system comprises an extensive network of Lower Cretaceous sandstone reservoirs juxtaposed grabens and half grabens extending some 160 km by normal faulting against Upper Cretaceous synrift from the Anah graben in western Iraq to the sources and seals. Palmyride fold belt in central Syria, where it becomes more subdued. The youngest prerift rocks are presently at a maximum depth of about 5 km. INTRODUCTION Based primarily on interpretation of 1500 km of seismic reflection profiles and data from 35 wells, Recent detailed studies on a number of continen- we mapped a complex network of numerous tal rifts have shed considerable light on the archi- branching normal and strike-slip faults, generally tecture and evolution of these types of basins (e.g., striking northwest and west-northwest. Both Rosendahl, 1987; Morley, 1995). Continental rifts branched and single-strand linear normal faults of hosting major hydrocarbon accumulations include generally steep dip, as well as positive and negative the North Sea (e.g., Stewart et al., 1992), Gulf of flower structures, are manifest on seismic sections. -
Geological Evolution of the Red Sea: Historical Background, Review and Synthesis
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/277310102 Geological Evolution of the Red Sea: Historical Background, Review and Synthesis Chapter · January 2015 DOI: 10.1007/978-3-662-45201-1_3 CITATIONS READS 6 911 1 author: William Bosworth Apache Egypt Companies 70 PUBLICATIONS 2,954 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: Near and Middle East and Eastern Africa: Tectonics, geodynamics, satellite gravimetry, magnetic (airborne and satellite), paleomagnetic reconstructions, thermics, seismics, seismology, 3D gravity- magnetic field modeling, GPS, different transformations and filtering, advanced integrated examination. View project Neotectonics of the Red Sea rift system View project All content following this page was uploaded by William Bosworth on 28 May 2015. The user has requested enhancement of the downloaded file. All in-text references underlined in blue are added to the original document and are linked to publications on ResearchGate, letting you access and read them immediately. Geological Evolution of the Red Sea: Historical Background, Review, and Synthesis William Bosworth Abstract The Red Sea is part of an extensive rift system that includes from south to north the oceanic Sheba Ridge, the Gulf of Aden, the Afar region, the Red Sea, the Gulf of Aqaba, the Gulf of Suez, and the Cairo basalt province. Historical interest in this area has stemmed from many causes with diverse objectives, but it is best known as a potential model for how continental lithosphere first ruptures and then evolves to oceanic spreading, a key segment of the Wilson cycle and plate tectonics. -
University of Florida Thesis Or Dissertation Formatting
UNDERSTANDING CARNIVORAN ECOMORPHOLOGY THROUGH DEEP TIME, WITH A CASE STUDY DURING THE CAT-GAP OF FLORIDA By SHARON ELIZABETH HOLTE A DISSERTATION PRESENTED TO THE GRADUATE SCHOOL OF THE UNIVERSITY OF FLORIDA IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY UNIVERSITY OF FLORIDA 2018 © 2018 Sharon Elizabeth Holte To Dr. Larry, thank you ACKNOWLEDGMENTS I would like to thank my family for encouraging me to pursue my interests. They have always believed in me and never doubted that I would reach my goals. I am eternally grateful to my mentors, Dr. Jim Mead and the late Dr. Larry Agenbroad, who have shaped me as a paleontologist and have provided me to the strength and knowledge to continue to grow as a scientist. I would like to thank my colleagues from the Florida Museum of Natural History who provided insight and open discussion on my research. In particular, I would like to thank Dr. Aldo Rincon for his help in researching procyonids. I am so grateful to Dr. Anne-Claire Fabre; without her understanding of R and knowledge of 3D morphometrics this project would have been an immense struggle. I would also to thank Rachel Short for the late-night work sessions and discussions. I am extremely grateful to my advisor Dr. David Steadman for his comments, feedback, and guidance through my time here at the University of Florida. I also thank my committee, Dr. Bruce MacFadden, Dr. Jon Bloch, Dr. Elizabeth Screaton, for their feedback and encouragement. I am grateful to the geosciences department at East Tennessee State University, the American Museum of Natural History, and the Museum of Comparative Zoology at Harvard for the loans of specimens. -
Egypt in the Twenty-First Century: Petroleum Potential in Offshore Trends
GeoArabia, Vol. 6, No. 2, 2000 Gulf PetroLink, Bahrain Petroleum Potential in Offshore Trends, Egypt Egypt in the Twenty-First Century: Petroleum Potential in Offshore Trends John C. Dolson, Mark V. Shann, BP Amoco Corporation, Egypt Sayed I. Matbouly, Egyptian General Petroleum Corporation Hussein Hammouda and Rashed M. Rashed, Gulf of Suez Petroleum Company ABSTRACT Since the onshore discovery of oil in the Eastern Desert in 1886, the petroleum industry in Egypt has accumulated reserves of more than 15.5 billion barrels of oil equivalent. An understanding of the tectono-stratigraphic history of each major basin, combined with drilling history and field-size distributions, justifies the realization of the complete replacement of these reserves in the coming decades. Most of the increase in reserves will be the result of offshore exploration. In addition to the 25 trillion cubic feet already discovered, the offshore Mediterranean may hold 64 to 84 trillion cubic feet and the onshore Western Desert may contribute 15 to 30 trillion cubic feet in new gas resources. Many of the new fields are expected to be in the giant-field class that contains greater than 100 million barrels of oil equivalent. Challenges include sub-salt imaging, market constraints for predominantly gas resources and economic constraints imposed by the high cost of development of the current deep- water gas discoveries that are probably unique worldwide. The offshore Gulf of Suez may yield an additional 1.5 to 3.3 billion barrels of oil equivalent, but it continues to be technologically constrained by poor-quality seismic data. Advances in multiple suppression and development of new ‘off-structure’ play concepts with higher quality seismic data should result in continual new pool discoveries. -
(CARNIVORA: AMPHICYONIDAE) from the UPPER MIOCENE of BATALLONES-1, MADRID, SPAIN by STE´ PHANE PEIGNE´ *, MANUEL J
[Palaeontology, Vol. 51, Part 4, 2008, pp. 943–965] A NEW AMPHICYONINE (CARNIVORA: AMPHICYONIDAE) FROM THE UPPER MIOCENE OF BATALLONES-1, MADRID, SPAIN by STE´ PHANE PEIGNE´ *, MANUEL J. SALESA , MAURICIO ANTO´ N and JORGE MORALES *Muse´um national d’Histoire naturelle, De´partement Histoire de la Terre, USM 0203 ⁄ UMR 5143 Pale´obiodiversite´ et Pale´oenvironnement, CP 38, 8, rue Buffon, 75231 Paris cedex 05, France; e-mail: [email protected] Departamento de Paleobiologı´a, Museo Nacional de Ciencias Naturales-CSIC, c ⁄ Jose´ Gutie´rrez Abascal, 2, 28006 Madrid, Spain; e-mails: [email protected], [email protected], [email protected] Typescript received 4 July 2007; accepted in revised form 17 September 2007 Abstract: The vertebrate community of the late Miocene anceps gen. et sp. nov., is markedly distinct from all other locality of Batallones-1, Madrid Province, Spain, is mainly known Amphicyoninae, specifically in its hypercarnivorous composed of mammals of the order Carnivora, which rep- features (strongly compressed upper canines, absence of resents 98 per cent of the total number of macro-mammal dP1 ⁄ dp1 and P2 ⁄ p2, single-rooted p3, absence of a meta- fossils. Here, we describe craniodental remains of approxi- conid on the lower molars, and reduction of M2 relative mately 12 individuals of a new, highly specialized member to M1). of the Amphicyonidae, previously assigned to Amphicyon sp. cf. A. castellanus. A phylogenetic analysis of Amphicy- Key words: Carnivora, Amphicyonidae, Spain, Miocene, oninae shows that this new form, named Magericyon Vallesian, carnivore trap, Batallones. Since 1991, the localities of Cerro de los Batallones in This study describes the remains of another well-known Madrid Province, Spain (Text-fig. -
The Oligo–Miocene Closure of the Tethys Ocean and Evolution of the Proto‑Mediterranean Sea Adi Torfstein1,2* & Josh Steinberg3
www.nature.com/scientificreports OPEN The Oligo–Miocene closure of the Tethys Ocean and evolution of the proto‑Mediterranean Sea Adi Torfstein1,2* & Josh Steinberg3 The tectonically driven Cenozoic closure of the Tethys Ocean invoked a signifcant reorganization of oceanic circulation and climate patterns on a global scale. This process culminated between the Mid Oligocene and Late Miocene, although its exact timing has remained so far elusive, as does the subsequent evolution of the proto-Mediterranean, primarily due to a lack of reliable, continuous deep-sea records. Here, we present for the frst time the framework of the Oligo–Miocene evolution of the deep Levant Basin, based on the chrono-, chemo- and bio- stratigraphy of two deep boreholes from the Eastern Mediterranean. The results reveal a major pulse in terrigeneous mass accumulation rates (MARs) during 24–21 Ma, refecting the erosional products of the Red Sea rifting and subsequent uplift that drove the collision between the Arabian and Eurasian plates and the efective closure of the Indian Ocean-Mediterranean Seaway. Subsequently, the proto-Mediterranean experienced an increase in primary productivity that peaked during the Mid‑Miocene Climate Optimum. A region‑ wide hiatus across the Serravallian (13.8–11.6 Ma) and a crash in carbonate MARs during the lower Tortonian refect a dissolution episode that potentially marks the earliest onset of the global middle to late Miocene carbonate crash. Global climate oscillations during the Miocene refect major events in the Earth’s history such as the closure of the Indian Ocean-Mediterranean Seaway (IOMS), Mid-Miocene Climate Optimum (MMCO), and the glacia- tion of Antarctica1. -
Bulletin Analytique
Ministère Des Mines Agence du Service Géologique de l'Algérie Division Géo-Information Département Documentation Bibliothèque des Sciences de la Terre Bulletin Analytique NALES & TIO IN A TE N R S N N A O I T I T O A N C A I L L E B S U P 2020 MINISTERE DES MINES AGENCE DU SERVICE GEOLOGIQUE DE L’ALGERIE Division Géo-Information Département Documentation BIBLIOTHEQUE DES SCIENCES DE LA TERRE PRESENTATION La Bibliothèque des Sciences de la Terre (BST) de la Division Géo-Information /Département Documentation, placée sous l’autorité de l’Agence du Service Géologique de l’Algérie, diffuse annuellement 1 numéro du Bulletin Analytique fournissant aux usagers des références bibliographiques de publications reçues par la BST dans le cadre des échanges avec les organismes étrangers, d’abonnements et d’ouvrages de bases acquis. La Bibliothèque des Sciences de la Terre est ouverte au public pour consultation de son fonds documentaire aux horaires suivants : du Dimanche au Jeudi 8h 00 - 12h 00 13h 00 -16h 00 Agence du Service Géologique de l’Algérie Bibliothèque des Sciences de la Terre 18A, Avenue Mustapha EL Ouali (ex Debussy) - Alger 16.000 BULLETIN ANALYTIQUE 2020 S O M M A I R E Energie…………………………………………………………………………………….. 5 Géologie Structurale……………………………………………………………………… 6 Stratigraphie………………………………………………………………………………. 8 Sédimentologie…………………………………………………………………………….. 9 Géologie régionale – Cartes………………………………………………………………. 12 Paléontologie……………………………………………………………………………….. 15 Minéralogie…………………………………………………………………………………. 21 Géologie Minière……………………………………………………………………………. 23 Géochimie…………………………………………………………………………………… 26 Hydrologie…………………………………………………………………………………… 29 Géophysique…………………………………………………………………………………. 31 Géomorphologie……………………………………………………………………………… 32 Environnement……………………………………………………………………………….. 34 INDEX DES REVUES……………………………………………………………………….. 35 3 BULLETIN ANALYTIQUE 2020 ENERGIE 1 : Evaluation of source rock potential and hydrocarbon composition of oil sand and associated clay deposits from the Eastern Dahomey Basin, Nigeria. -
Plate Kinematics of the Afro-Arabian Rift System with an Emphasis on the Afar Depression
Scholars' Mine Doctoral Dissertations Student Theses and Dissertations Fall 2012 Plate kinematics of the Afro-Arabian Rift System with an emphasis on the Afar Depression Helen Carrie Bottenberg Follow this and additional works at: https://scholarsmine.mst.edu/doctoral_dissertations Part of the Geology Commons, and the Geophysics and Seismology Commons Department: Geosciences and Geological and Petroleum Engineering Recommended Citation Bottenberg, Helen Carrie, "Plate kinematics of the Afro-Arabian Rift System with an emphasis on the Afar Depression" (2012). Doctoral Dissertations. 2237. https://scholarsmine.mst.edu/doctoral_dissertations/2237 This thesis is brought to you by Scholars' Mine, a service of the Missouri S&T Library and Learning Resources. This work is protected by U. S. Copyright Law. Unauthorized use including reproduction for redistribution requires the permission of the copyright holder. For more information, please contact [email protected]. iii iv PLATE KINEMATICS OF THE AFRO-ARABIAN RIFT SYSTEM WITH EMPHASIS ON THE AFAR DEPRESSION, ETHIOPIA by HELEN CARRIE BOTTENBERG A DISSERTATION Presented to the Faculty of the Graduate School of the MISSOURI UNIVERSITY OF SCIENCE & TECHNOLOGY In Partial Fulfillment of the Requirements for the Degree DOCTOR OF PHILOSOPHY in GEOLOGY & GEOPHYSICS 2012 Approved by Mohamed Abdelsalam, Advisor Stephen Gao Leslie Gertsch John Hogan Allison Kennedy Thurmond v 2012 Helen Carrie Bottenberg All Rights Reserved iii PUBLICATION DISSERTATION OPTION This dissertation has been prepared in the style utilized by Geosphere and The Journal of African Earth Sciences. Pages 6-41 and Pages 97-134 will be submitted for separate publications in Geosphere and pages 44-96 will be submitted to Journal of African Earth Sciences iv ABSTRACT This work utilizes the Four-Dimensional Plates (4DPlates) software, and Differential Interferometric Synthetic Aperture Radar (DInSAR) to examine plate-scale, regional- scale and local-scale kinematics of the Afro-Arabian Rift System with emphasis on the Afar Depression in Ethiopia. -
Back Matter (PDF)
Index Page numbers in italic denote figures. Page numbers in bold denote tables. Accra Plains Migmatite, correlation with Me´dio Coreau´ Bafia Group 86 domain 102–103, 114 Bahia–Gabon continental bridge 153, 154 Adamastor ocean Baixo Araguaia Supergroup 174, 299 closure 260, 265, 269, 270, 271, 271, 273 geochronology 184, 189, 190, 191 subduction 229, 231 Baltica Adamawa fault 92 palaeogeography 13–16, 14, 15, 17,22–23 Adamawa–Yade´ domain 85, 85, 87, 88,90–91 palaeomagnetic poles 10, 11 Afagados do Ingrazeira fault 72 Bambui Group 165, 201, 206 A´ gua Clara domain 241, 242 Bandeirinha Formation 36, 36, 37 A´ guas Belas–Caninde´ suite 80, 81 Bangweulu block 33, 43–45 Akanyaru Supergroup 33, 41–43, 45 Baoule´ –Mossi domain 142–144 Albian gap 379, 382, 384, 392 Barro Alto complex 204 Ale´m Paraı´ba shear zone 222 basalt, Brazilian margin 373 Algodo˜es Unit 53 basins Alto Moxoto´ terrane 72, 77, 92 sag Alto Pajeu´ terrane 72, 73, 77, 78, 92 Espirito Santo Basin 379 Amazonia Sa˜o Francisco craton 33, 34, 35–36, 39 palaeogeography 13–16, 14, 15, 16, 17, 21, 22–23 salt, Brazilian margin 366–370, 367, 375 palaeomagnetic poles 12,13 sedimentary Amazonian craton 102 Borborema Province 56 geochronology 177, 189, 191 Garupi Belt 141 Andrelaˆndia Group 164, 202, 205, 217 Parana´ –Cape–Karoo 319–337 Angola craton 4, 5, 223, 224, 225–226 rift, Brazilian margin, uplifted flanks 383–387 correlation with Cabo Frio terrane 292 Sa˜o Francisco–Congo craton 33–46 Apiaı´ terrane 214, 218, 221, 222–223, 229 Sa˜o Luı´s craton 140, 141 Apparent Polar Wander Path