A Fossil Locality Predictive Model for the Early Cretaceous Cedar Mountain Formation, Utah, Usa

Total Page:16

File Type:pdf, Size:1020Kb

A Fossil Locality Predictive Model for the Early Cretaceous Cedar Mountain Formation, Utah, Usa A FOSSIL LOCALITY PREDICTIVE MODEL FOR THE EARLY CRETACEOUS CEDAR MOUNTAIN FORMATION, UTAH, USA A THESIS PRESENTED TO THE DEPARTMENT OF HUMANITIES AND SOCIAL SCIENCE IN CANDIDACY FOR THE DEGREE OF MASTER OF SCIENCE By DANIEL BURK NORTHWEST MISSOURI STATE UNIVERSITY MARYVILLE, MISSOURI OCTOBER, 2014 FOSSIL LOCALITY PREDICTIVE MODEL A Fossil Locality Predictive Model for the Early Cretaceous Cedar Mountain Formation, Utah, USA Daniel Burk Northwest Missouri State University THESIS APPROVED Thesis Advisor, Dr. Yi-Hwa Wu Date Dr. Ming-Chih Hung Date Dr. John P. Pope Date Dean of Graduate School Date A Fossil Locality Predictive Model for the Early Cretaceous Cedar Mountain Formation, Utah, USA Abstract Hard work and chance are nearly always among the deciding factors in finding new, important, and productive paleontological localities. Fossil locality predictive models have the potential to reduce unproductive field time and maximize hard work thus increasing the chances researchers have to find important localities. This study uses remotely sensed data to design and test a fossil locality predictive model for the Early Cretaceous Cedar Mountain Formation. Landsat 8 OLI/TIRS data from known localities were summarized, reclassified and used in a weighted suitability analysis to categorize fossil locality potential of the study area. Field work was conducted to test model functionality. Field observations were used to refine the weighted suitability analysis. Landsat 8 OLI/TIRS data alone offers a less accurate prescription of fossil locality potential. Additional physical and environmental factors play a role in determining the chance of finding fossils. Slope degree and aspect data from known localities were summarized and analyzed to further refine the model. The usefulness of fossil locality predictive models is dependent upon the quality of input data and methods used to determine fossil locality potential. In order to fully determine the quality of a fossil locality predictive model, field work testing the model must be conducted. iii TABLE OF CONTENTS LIST OF FIGURES .......................................................................................................vi LIST OF TABLES .........................................................................................................vii ACKNOWLEDGEMENTS ..............................................................................................viii CHAPTER 1: INTRODUCTION .....................................................................................1 Statement of the Problem ..............................................................................1 Background and Need ..................................................................................1 Justification/Rationale ..................................................................................3 Research Objectives ......................................................................................5 Study Area .....................................................................................................5 CHAPTER 2: LITERATURE REVIEW ..........................................................................8 CHAPTER 3: CONCEPTUAL FRAMEWORK AND METHODOLOGY .............................12 Data Sources .................................................................................................12 Landsat 8 OLI/TIRS Imagery .............................................................12 Geologic Maps ...................................................................................13 BYU Fossil Localities ........................................................................15 Digital Elevation Model (DEM) ........................................................16 Published Fossil Localities ................................................................17 Research Methodology ..................................................................................17 Overview ............................................................................................17 Summary of Fossil Locality Spectral Reflectance .............................19 Weighted Suitability Analysis ............................................................21 Field Test of Model ............................................................................22 CHAPTER 4: ANALYSIS RESULTS AND DISCUSSION ..................................................25 Problems with Model ....................................................................................25 iv Initially Observed Problems ..............................................................25 Problems Observed Through Field Work ..........................................26 Revised Weighted Suitability Analysis .........................................................27 Revised Reclassification.....................................................................27 Revised Weights .................................................................................27 Testing the Revised Model .................................................................30 Refined Model: Additional Parameters ........................................................31 Surface Aspect ....................................................................................31 Surface Slope .....................................................................................33 Refined Model Results........................................................................35 Additional Issues ...........................................................................................36 Geologic Map Accuracy ....................................................................36 Unresolved Problems with the Model ................................................41 CHAPTER 5: CONCLUSION ........................................................................................44 LIST OF REFERENCES ................................................................................................47 v LIST OF FIGURES Figure 1: Early Cretaceous Cedar Mountain Formation surface exposure, elevation, and fossil localities ................................................................................................... 7 Figure 2: Landsat 8 natural color composite image centered on the Cedar Mountain Formation ................................................................................................................................. 12 Figure 3: Surface coverage of 1:24,000 scale geological maps ............................................. 14 Figure 4: Slope and Aspect data for the Cedar Mountain Formation................................... 16 Figure 5: Simplified flowchart showing methodology .......................................................... 18 Figure 6: Differences of means between fossil localities and Cedar Mountain Formation (X1-X2) ....................................................................................................................... 20 Figure 7: Weighted suitability analysis results ...................................................................... 22 Figure 8: Photos of the ten test sites. Numbers correspond to those in Table 6 ................ 24 Figure 9: Number of cells assigned to each fossil potential value for the model ................. 26 Figure 10: Revised weighted suitability analysis results ....................................................... 28 Figure 11: Number of cells assigned to each fossil potential value for the revised model ................................................................................................................................. 29 Figure 12: Comparison of aspects between the entire Cedar Mountain Formation and BYU fossil localities .................................................................................................. 32 Figure 13: Comparison of slopes between the entire Cedar Mountain Formation and BYU fossil localities .......................................................................................................... 34 Figure 14: Refined model results .......................................................................................... 35 Figure 15: Detailed comparison of model versions .............................................................. 36 Figure 16: Detailed comparison of small and large scale maps ............................................ 38 Figure 17: Detailed comparison of geologic maps in the area surrounding the Dalton Wells Dinosaur Quarry ....................................................................................................... 40 vi LIST OF TABLES Table 1: Summary of Landsat OLI/TIRS bands (adapted from Irons et al. 2012) .................. 13 Table 2: Summary of Geologic Maps used in this study ....................................................... 15 Table 3: Summary of Landsat OLI/TIRS spectral reflectance values for BYU fossil localities ................................................................................................................................. 20 Table 4: Summary of Landsat OLI/TIRS spectral reflectance values for the Cedar Mountain Fm ............................................................................................................................ 20 Table 5: Reclassified values for OLI/TIRS bands used in weighted suitability analysis ......... 21 Table 6: Suitability analysis weights for model ..................................................................... 21 Table 7: Summary of field test results
Recommended publications
  • A New Microvertebrate Assemblage from the Mussentuchit
    A new microvertebrate assemblage from the Mussentuchit Member, Cedar Mountain Formation: insights into the paleobiodiversity and paleobiogeography of early Late Cretaceous ecosystems in western North America Haviv M. Avrahami1,2,3, Terry A. Gates1, Andrew B. Heckert3, Peter J. Makovicky4 and Lindsay E. Zanno1,2 1 Department of Biological Sciences, North Carolina State University, Raleigh, NC, USA 2 North Carolina Museum of Natural Sciences, Raleigh, NC, USA 3 Department of Geological and Environmental Sciences, Appalachian State University, Boone, NC, USA 4 Field Museum of Natural History, Chicago, IL, USA ABSTRACT The vertebrate fauna of the Late Cretaceous Mussentuchit Member of the Cedar Mountain Formation has been studied for nearly three decades, yet the fossil-rich unit continues to produce new information about life in western North America approximately 97 million years ago. Here we report on the composition of the Cliffs of Insanity (COI) microvertebrate locality, a newly sampled site containing perhaps one of the densest concentrations of microvertebrate fossils yet discovered in the Mussentuchit Member. The COI locality preserves osteichthyan, lissamphibian, testudinatan, mesoeucrocodylian, dinosaurian, metatherian, and trace fossil remains and is among the most taxonomically rich microvertebrate localities in the Mussentuchit Submitted 30 May 2018 fi fi Accepted 8 October 2018 Member. To better re ne taxonomic identi cations of isolated theropod dinosaur Published 16 November 2018 teeth, we used quantitative analyses of taxonomically comprehensive databases of Corresponding authors theropod tooth measurements, adding new data on theropod tooth morphodiversity in Haviv M. Avrahami, this poorly understood interval. We further provide the first descriptions of [email protected] tyrannosauroid premaxillary teeth and document the earliest North American record of Lindsay E.
    [Show full text]
  • PALEONTOLOGICAL TECHNICAL REPORT: 6Th AVENUE and WADSWORTH BOULEVARD INTERCHANGE PHASE II ENVIRONMENTAL ASSESSMENT, CITY of LAKEWOOD, JEFFERSON COUNTY, COLORADO
    PALEONTOLOGICAL TECHNICAL REPORT: 6th AVENUE AND WADSWORTH BOULEVARD INTERCHANGE PHASE II ENVIRONMENTAL ASSESSMENT, CITY OF LAKEWOOD, JEFFERSON COUNTY, COLORADO Prepared for: TEC Inc. 1746 Cole Boulevard, Suite 265 Golden, CO 80401 Prepared by: Paul C. Murphey, Ph.D. and David Daitch M.S. Rocky Mountain Paleontology 4614 Lonespur Court Oceanside, CA 92056 303-514-1095; 760-758-4019 www.rockymountainpaleontology.com Prepared under State of Colorado Paleontological Permit 2007-33 January, 2007 TABLE OF CONTENTS 1.0 SUMMARY............................................................................................................................. 3 2.0 INTRODUCTION ................................................................................................................... 4 2.1 DEFINITION AND SIGNIFICANCE OF PALEONTOLOGICAL RESOURCES........... 4 3.0 METHODS .............................................................................................................................. 6 4.0. LAWS, ORDINANCES, REGULATIONS AND STANDARDS......................................... 7 4.1. Federal................................................................................................................................. 7 4.2. State..................................................................................................................................... 8 4.3. County................................................................................................................................. 8 4.4. City.....................................................................................................................................
    [Show full text]
  • How Old Is Old? (.Pdf)
    How Old is Old? Purpose: This lesson will help students visualize the geologic time scale and identify when and where regional features were formed in the Rogue Valley. Objectives: Time Required: 1.5 hours (can be Students will: broken into 2 class periods) Identify the point in time when their assigned Appropriate grades: 6th-8th geological formation was formed by calculating NGSS and Common Core Standards: how many centimeters from the end of the MS-ESS2-2: Construct an explanation based ribbon their tag should be placed. on evidence for how geoscience processes Teach the class about their assigned geological have changed Earth's surface at varying time formations by conducting research about when and spatial scales. they were formed, how they were formed, CCSS.ELA-LITERACY.SL.6-8.4: Present claims where they are located, and what they are made and findings, emphasizing salient points in a of, and preparing visual presentations in small focused, coherent manner with pertinent groups. descriptions, facts, details, and examples; use appropriate eye contact, adequate Materials: volume, and clear pronunciation. CCSS.ELA-LITERACY.SL.6-8.5: Include Time scale ribbon (1) multimedia components and visual displays Time period tags (19) in presentations to clarify claims and “Geology of Jackson County, Oregon” booklets findings and emphasize salient points. (5) Geological formation half sheets (1 for each group with the name of their formation on it) Poster boards (not provided) Markers (not provided) Activity: Introduction Prep: cut the geological formation half sheets along the solid line in the middle of the page. Each group of students will get a half sheet with the name of their geological formation.
    [Show full text]
  • Geological Formation Educational Hand Sample Collection Content Last Updated 06/30/2010
    CT Geological Survey Geological Formation Educational Hand Sample Collection Content last updated 06/30/2010 TOWN Sample Numer Geological Description Formation Barkhamsted 19-9-1 Єh Cambrian "Waramaug Formation", Hoosac Schist, West Hill Road, New Hartford, 2 samples. Quartzplagioclase- biotite schist and gneissic schist. Bethel 92-4-1 Og Collected from Huntington State Park, site of large tourmaline 76-9-1 OCs Inwood? Marble from W side of stream just below Cameron's Line 76-9-2 Or Sheared Hartland? from E side of stream just above Cameron's Line Bozrah 71-5 Otay Collected from intersection of South and Bishop Rds, Bozrah Branford 97-1 Zsc & Pn Stony Creek Quarry Granite 97-6 Zp, Zsc & Pn From Red Hill Quarry, Stony Creek Preserve, Branford Bridgeport 109-1 Ohb Collected in Beardsley Park, Bridgeport Burlington 35-5-1 DSt Straits Schist, collected on road cut for entrance of side road on W side of Maine Rd Canterbury 57-6-1 Dc Canterbury Gneiss, Note Muskovite and garnet? 57-6-2 SOh Meta siltstone/Hornfels? Mapped as hCS on GQ 392, Collected just W of pond, low outcrops Canterbury is just to the W of the outcrop, inclusions of this rock and a very fine grained biotite schist are found in Canterbury. This rock is quite massive with n Chester 84-7 Dc In woods SW of Chester Elementary School, Ridge Rd, Chester 84-1 b SOh Biotite Gneiss and schist, E side of northbound entrance ramp intersection of Rt 9 and 148 84-1 c SOh Biotite Gneiss and schist, E side of northbound entrance ramp intersection of Rt 9 and 148 84-1 a SOh Biotite Gneiss
    [Show full text]
  • Oil and Gas Plays Ute Moutnain Ute Reservation, Colorado and New Mexico
    Ute Mountain Ute Indian Reservation Cortez R18W Karle Key Xu R17W T General Setting Mine Xu Xcu 36 Can y on N Xcu McElmo WIND RIVER 32 INDIAN MABEL The Ute Mountain Ute Reservation is located in the northwest RESERVATION MOUNTAIN FT HALL IND RES Little Moude Mine Xcu T N ern portion of New Mexico and the southwestern corner of Colorado UTE PEAK 35 N R16W (Fig. UM-1). The reservation consists of 553,008 acres in Montezu BLACK 666 T W Y O M I N G MOUNTAIN 35 R20W SLEEPING UTE MOUNTAIN N ma and La Plata Counties, Colorado, and San Juan County, New R19W Coche T Mexico. All of these lands belong to the tribe but are held in trust by NORTHWESTERN 34 SHOSHONI HERMANO the U.S. Government. Individually owned lands, or allotments, are IND RES Desert Canyon PEAK N MESA VERDE R14W NATIONAL GREAT SALT LAKE W Marble SENTINEL located at Allen Canyon and White Mesa, San Juan County, Utah, Wash Towaoc PARK PEAK T and cover 8,499 acres. Tribal lands held in trust within this area cov Towaoc River M E S A 33 1/2 N er 3,597 acres. An additional forty acres are defined as U.S. Govern THE MOUND R15W SKULL VALLEY ment lands in San Juan County, Utah, and are utilized for school pur TEXAS PACIFIC 6-INCH OIL PIPELINE IND RES UNITAH AND OURAY INDIAN RESERVATION Navajo poses. W Ramona GOSHUTE 789 The Allen Canyon allotments are located twelve miles west of IND RES T UTAH 33 Blanding, Utah, and adjacent to the Manti-La Sal National Forest.
    [Show full text]
  • On the Distribution of Utah's Hanging Gardens
    Great Basin Naturalist Volume 49 Number 1 Article 1 1-31-1989 On the distribution of Utah's hanging gardens Stanley L. Welsh Brigham Young University Follow this and additional works at: https://scholarsarchive.byu.edu/gbn Recommended Citation Welsh, Stanley L. (1989) "On the distribution of Utah's hanging gardens," Great Basin Naturalist: Vol. 49 : No. 1 , Article 1. Available at: https://scholarsarchive.byu.edu/gbn/vol49/iss1/1 This Article is brought to you for free and open access by the Western North American Naturalist Publications at BYU ScholarsArchive. It has been accepted for inclusion in Great Basin Naturalist by an authorized editor of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. The Great Basin Naturalist Published at Provo, Utah, by Brigham Young University ISSN 0017-3614 Volume 49 31 January 1989 No. 1 ON THE DISTRIBUTION OF UTAH'S HANGING GARDENS Stanley L. Welsh 1 Abstract. —This is a summary monograph of the hanging gardens as they occur in the Colorado River and Virgin River portions of the Colorado Plateau in Utah. Discussed in this paper are the hanging gardens, their geography, geomorphology, aspects of distribution and diversity, and principal vascular and algal plant species. Animal trapping studies and plant productivity aspects are reviewed. The sea of aridity that overlies southern tively recent origin, geologically speaking Utah and vicinity is broken by seasonal influ- (Hintze 1972). ences and by the dendritic trenches of the The geological strata are remarkably evi- Colorado River and its tributaries. The effects dent in this arid setting, where vegetative of the river are restricted to its banks and cover is thin and where rate of soil develop- adjacent alluvial terraces; the riparian vegeta- ment is exceeded by processes of erosion.
    [Show full text]
  • A Jurassic Basal Eusauropod Clade from Iberia Finds Refuge In
    View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by UCL Discovery Descendants of the Jurassic turiasaurs from Iberia found refuge in the Early Cretaceous of western USA Rafael Royo-Torres, Paul Upchurch, James I. Kirkland, Donald D. DeBlieux, John R. Foster, Alberto Cobos, Luis Alcalá Supplementary Information: I. Abbreviations section II. Geological setting of the Doelling’s Bowl bonebed III. Phylogenetic analyses and list of synapomorphies IV. Holotype of Mierasaurus V. Measurements VI. References I. Abbreviations section BYU (Museum of Paleontology of Brigham Young University, Provo, Utah USA). DBBB Doelling’s Bowl bonebed; DBGI Doelling’s Bowl site; J-K Jurassic- Cretaceous transition; Ma million years ago; My million years; MPT most parsimonious trees; RD name for every dinosaur site from Riodeva in Teruel (Spain); TL Tree length; UMNH the Natural History Museum of Utah (USA); UGS Utah Geological Survey (USA). Anatomical abbreviations: bt basal tubera; bo basioccipital; bpt basipterygoid process; ca crista antotica; ct crista tuberalis; f frontal; fme fenestra metotic; fv fenestra vestivuli (=fenestra ovalis); osc otosphenoidal crest (= crista prootica); p parietal; pa parapophysis; prf prefontal; stf supratemporal fossa; so supraoccipital; eo exoccipital- opisthotic; bo basioccipital; popr paraoccipital process; cranial nerves: I olfactory nerve; II optic nerve; III oculomotor nerve; IV trochlear nerve; V trigeminal nerve (ophthalmic, maxillary, mandibular); VI abductor or abducens nerve; VII facialis nerve; VIII vestibulocochlear nerve. Abbreviations for laminae vertebral: acpl anterior centroparapophyseal lamina; ant. spdl anterior spinodiapophyseal lamina; cprl 1 centroprezygapophyseal lamina; cpol centropostzygapophyseal lamina; pcdl posterior centrodiapophyseal lamina; post. spdl posterior spinodiapophyseal lamina; ppdl paradiapophyseal lamina; prdl prezygodiapophyseal lamina; spol spinopostzygapophyseal lamina.
    [Show full text]
  • Late Cretaceous Stratigraphy and Vertebrate Faunas of the Markagunt, Paunsaugunt, and Kaiparowits Plateaus, Southern Utah
    GEOLOGY OF THE INTERMOUNTAIN WEST an open-access journal of the Utah Geological Association Volume 3 2016 LATE CRETACEOUS STRATIGRAPHY AND VERTEBRATE FAUNAS OF THE MARKAGUNT, PAUNSAUGUNT, AND KAIPAROWITS PLATEAUS, SOUTHERN UTAH Alan L. Titus, Jeffrey G. Eaton, and Joseph Sertich A Field Guide Prepared For SOCIETY OF VERTEBRATE PALEONTOLOGY Annual Meeting, October 26 – 29, 2016 Grand America Hotel Salt Lake City, Utah, USA Post-Meeting Field Trip October 30–November 1, 2016 © 2016 Utah Geological Association. All rights reserved. For permission to copy and distribute, see the following page or visit the UGA website at www.utahgeology.org for information. Email inquiries to [email protected]. GEOLOGY OF THE INTERMOUNTAIN WEST an open-access journal of the Utah Geological Association Volume 3 2016 Editors UGA Board Douglas A. Sprinkel Thomas C. Chidsey, Jr. 2016 President Bill Loughlin [email protected] 435.649.4005 Utah Geological Survey Utah Geological Survey 2016 President-Elect Paul Inkenbrandt [email protected] 801.537.3361 801.391.1977 801.537.3364 2016 Program Chair Andrew Rupke [email protected] 801.537.3366 [email protected] [email protected] 2016 Treasurer Robert Ressetar [email protected] 801.949.3312 2016 Secretary Tom Nicolaysen [email protected] 801.538.5360 Bart J. Kowallis Steven Schamel 2016 Past-President Jason Blake [email protected] 435.658.3423 Brigham Young University GeoX Consulting, Inc. 801.422.2467 801.583-1146 UGA Committees [email protected] [email protected] Education/Scholarship
    [Show full text]
  • The End of the Sauropod Dinosaur Hiatus in North America
    Palaeogeography, Palaeoclimatology, Palaeoecology 297 (2010) 486–490 Contents lists available at ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo The end of the sauropod dinosaur hiatus in North America Michael D. D'Emic a,⁎, Jeffrey A. Wilson a, Richard Thompson b a Museum of Paleontology and Department of Geological Sciences, University of Michigan, 1109 Geddes Avenue, Ann Arbor, MI 48109–1079, USA b Department of Geosciences, University of Arizona, 1040 E 4th St, Tucson, AZ, 85721-0077, USA article info abstract Article history: Sauropod dinosaurs reached their acme in abundance and diversity in North America during the Late Received 4 February 2010 Jurassic. Persisting in lesser numbers into the Early Cretaceous, sauropods disappeared from the North Received in revised form 16 August 2010 American fossil record from the Cenomanian until the Campanian or Maastrichtian stage of the Late Accepted 30 August 2010 Cretaceous. This ca. 25–30 million-year long sauropod hiatus has been attributed to either a true extinction, Available online 19 September 2010 perhaps due to competition with ornithischian dinosaurs, or a false extinction, due to non-preservation of sediments bearing sauropods. The duration of the sauropod hiatus remains in question due to uncertainty in Keywords: fi Dinosaur the ages and af nities of the specimens bounding the observed gap. In this paper, we re-examine the Sauropod phylogenetic affinity of materials from Campanian-aged sediments of Adobe Canyon, Arizona that currently Titanosaur mark the end of the sauropod hiatus. Based on the original description of those remains and new specimens Alamosaurus from the same formation, we conclude that the Adobe Canyon vertebrae do not pertain to titanosaurs, but to Hadrosaur hadrosaurid dinosaurs.
    [Show full text]
  • DINOSAURS Contents the Director’S Perspective the Thumb-Spiked Iguanodontians—Dinosaurian Cows of the Early Cretaceous
    UTAH GEOLOGICAL SURVEY SURVEY NOTES Volume 45, Number 1 January 2013 UTAH'S NEW IGUANODONTIAN DINOSAURS Contents The Director’s Perspective The Thumb-Spiked Iguanodontians—Dinosaurian Cows of the Early Cretaceous ...........................1 Each year, the Utah Geological Survey of proven reserves Using Aquifers for Water Storage provides two chapters for the “Economic (barrels) to annual in Cache Valley ................................................ 4 Report to the Governor,” which is pub- oil production (bar- Establishing Baseline Water Quality in the lished by the Governor’s Office of Man- rels per year) has Southeastern Uinta Basin ............................. 6 agement and Budget in January. The two increased from GeoSights ............................................................. 8 chapters address energy and mineral typically 6 to 8 Glad You Asked .................................................... 9 industry trends in Utah during the past years of supply Energy News .......................................................10 year. The UGS also summarizes Utah’s prior to 2000, to Teacher’s Corner ................................................ 12 extractive resource industry trends in 18 years over the Survey News .......................................................13 an annual publication (recently pub- past three years. lished UGS Circular 115 summarizes 2011 In addition, annual New Publications ................................................13 trends). A key indicator we use to mea- oil production has sure the overall
    [Show full text]
  • Lithostratigraphic Units in the Drava Depression (Croatian and Hungarian Parts) – a Correlation
    Lithostratigraphic units in the Drava Depression (Croatian and Hungarian parts) – a correlation T. Malviæ and M. Cvetkoviæ ORIGINAL SCIENTIFIC PAPER The lithostratigraphic division and correlation is one of the most common stratigraphic divisions. It is strictly connected with lithological content of the rocks or deposits. Sometimes lithostratigraphic units, especially in rank of formations and members, can be approximately correlated with particular chronostratigraphic units in range of stages or sub-stages, i.e. lithosratigraphic units have synchronous borders. In other cases, the borders are asynchronous. Croatian and Hungarian lithostratigraphic units in the Drava Depression are analysed here as well as the possibility of their correlation. Such correlation scheme can be useful in comparison of different units, especially because the Croatian part is based on approximately synchronous, and Hungarian on asynchronous borders between units. Moreover, the Drava Depression in this region is an important hydrocarbon production province where lithostratigraphic correlation is widely used, even across state borders. The presented lithostratigraphic scheme, it's lithological descriptions and correlation could help in any geological research or evaluation in the entire analysed depression. Key words: lithostratigraphy, Drava Depression, Croatia, Hungary 1. Introduction The analysed chronostratigraphic and lithostrati- The entire Drava Depression covers the surface area of graphic units of the Drava Depression are based on nu- about 12 000 square km, where approximately 9 100 be- merous well and seismic data. There are several regional long to the Croatia (Figure 1). Generally, the Neogene and papers where ranks and lithostratigraphic units are de- Quaternary rocks and deposits defined the subsurface fined. In Croatian part the most famous source is ref.43 volume known as the Drava Depression.
    [Show full text]
  • Curriculum Vitae Christopher J
    C. J. Bell Curriculum Vitae Christopher J. Bell 10 January, 2012 Professor The University of Texas at Austin Department of Geological Sciences 1 University Station C1100 Austin, TX 78712-0254 (512) 471-7301 [email protected] Date and Place of Birth: 12 March, 1966; Marietta, Georgia, U.S.A. Education University of California, Berkeley, California. Department of Integrative Biology. Ph.D., 1997. Northern Arizona University, Flagstaff, Arizona. Quaternary Studies Program. M.S., 1990. The College of William and Mary in Virginia, Williamsburg, Virginia. Department of Geology. B.S., 1988. Professional Appointments - Current Sep., 2010 – present: Professor, Department of Geological Sciences, The University of Texas at Austin. April, 2007 – present: Research Associate, Department of Terrestrial Vertebrates, Western Australian Museum, Perth, Western Australia. Professional Appointments - Historical Sep., 2003 – Sept. 2010 : Associate Professor, Department of Geological Sciences, The University of Texas at Austin. September, 1997 - August, 2003: Assistant Professor, Department of Geological Sciences, The University of Texas at Austin. January, 1997 - May, 1997: Graduate Student Instructor, ‘Natural History of the Vertebrates,’ Department of Integrative Biology, U.C. Berkeley. August - December, 1996: Curatorial Assistant, Museum of Vertebrate Zoology, U.C. Berkeley. June - August, 1996: Graduate Student Curatorial Assistant, Museum of Paleontology, U.C. Berkeley. August - December, 1995: Graduate Student Instructor, ‘Morphology of the Vertebrate Skeleton,’ Department of Integrative Biology, U.C. Berkeley. June - August, 1995: Move Coordinator, Museum of Paleontology, U.C. Berkeley. January - May, 1995: Graduate Student Instructor, ‘The Age of Mammals,’ Department of Integrative Biology, U.C. Berkeley. 1 C. J. Bell August - December, 1994: Research Assistant to A. D. Barnosky, Porcupine Cave Project, Museum of Paleontology, U.
    [Show full text]