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Deep Groundwater and Potential Subsurface Habitats Beneath an Antarctic Dry Valley
ARTICLE Received 21 May 2014 | Accepted 2 Mar 2015 | Published 28 Apr 2015 DOI: 10.1038/ncomms7831 OPEN Deep groundwater and potential subsurface habitats beneath an Antarctic dry valley J.A. Mikucki1, E. Auken2, S. Tulaczyk3, R.A. Virginia4, C. Schamper5, K.I. Sørensen2, P.T. Doran6, H. Dugan7 & N. Foley3 The occurrence of groundwater in Antarctica, particularly in the ice-free regions and along the coastal margins is poorly understood. Here we use an airborne transient electromagnetic (AEM) sensor to produce extensive imagery of resistivity beneath Taylor Valley. Regional- scale zones of low subsurface resistivity were detected that are inconsistent with the high resistivity of glacier ice or dry permafrost in this region. We interpret these results as an indication that liquid, with sufficiently high solute content, exists at temperatures well below freezing and considered within the range suitable for microbial life. These inferred brines are widespread within permafrost and extend below glaciers and lakes. One system emanates from below Taylor Glacier into Lake Bonney and a second system connects the ocean with the eastern 18 km of the valley. A connection between these two basins was not detected to the depth limitation of the AEM survey (B350 m). 1 Department of Microbiology, University of Tennessee, Knoxville, Tennessee 37996, USA. 2 Department of Geosciences, Aarhus University, Aarhus 8000, Denmark. 3 Department of Earth and Planetary Sciences, University of California, Santa Cruz, California 95064, USA. 4 Environmental Studies Program, Dartmouth College, Hanover, New Hampshire 03755, USA. 5 Sorbonne Universite´s, UPMC Univ Paris 06, CNRS, EPHE, UMR 7619 Metis, 4 place Jussieu, Paris 75252, France. -
Tectonics and Seismicity of the Southern Washington Cascade Range
Bulletin of the Seismological Society of America, Vol. 86, No. 1A, pp. 1-18, February 1996 Tectonics and Seismicity of the Southern Washington Cascade Range by W. D. Stanley, S. Y. Johnson, A. I. Qamar, C. S. Weaver, and J. M. Williams Abstract Geophysical, geological, and seismicity data are combined to develop a transpressional strain model for the southern Washington Cascades region. We use this model to explain oblique fold and fault systems, transverse faults, and a linear seismic zone just west of Mt. Rainier known as the western Rainier zone. We also attempt to explain a concentration of earthquakes that connects the northwest-trend- ing Mount St. Helens seismic zone to the north-trending western Rainier zone. Our tectonic model illustrates the pervasive effects of accretionary processes, combined with subsequent transpressive forces generated by oblique subduction, on Eocene to present crustal processes, such as seismicity and volcanism. Introduction The southern Washington Cascades contains Mt. Rain- Geology of Western Washington ier, the most massive of the volcanoes in the Cascade Range magmatic arc (Fig. 1). Mr. Rainier is part of the triangle of The Puget Sound region and the western flank of the large stratovolcanoes in southem Washington that includes Cascade Range in southwestern Washington occupy a com- Mount St. Helens and Mt. Adams. Mount St. Helens expe- plex tectonic setting along the margin of two distinct crustal rienced a cataclysmic eruption in 1980 and is apparently blocks. Crust in the eastern block beneath the southwest younger than Mt. Rainier and Mt. Adams, both of which Washington Cascades is composed of Mesozoic and older exhibit more rounded profiles than the pointed, pre-1980 accreted terranes, volcanic arcs, and underplated magmatic Mount St. -
DEPARTMENT of ENVIRONMENTAL ENGINEERING and EARTH SCIENCES Department of Environmental Engineering and Earth Sciences Chairperson: Dr
DEPARTMENT OF ENVIRONMENTAL ENGINEERING AND EARTH SCIENCES Department of Environmental Engineering and Earth Sciences Chairperson: Dr. Marleen Troy Faculty Professors: Murthy, Troy, Whitman Associate Professors: Frederick Assistant Professor: Finkenbinder, Karimi, Karnae Lecturers: Kaster, McMonagle Laboratory Manager: McMonagle Office Assistant: Garrison The Department of Environmental Engineering and Earth Sciences (EEES) offers the following degree programs: the B.S. in Civil Engineering, the B.S. in Environmental Engineering; the B.S. in Environmental Science; the B.S. in Geology; and the B.A. in Earth and Environmental Science. EEES envisions future accreditation of the Civil Engineering program by EAC-ABET. The Environmental Engineering program is accredited by the EAC-ABET. The engineering programs incorporate a strong background in the fundamentals of engineering with a blend of science and advanced engineering courses. The Environmental Science program combines a foundation in the related sciences and primary earth reservoirs (water, land, air, and life) with concentrations in either Earth Science or Biology. The Geology program provides a comprehensive curriculum that includes the fundamentals of geology with courses responsive to the needs of industrial employment sectors. The Geology program meets the academic requirements for Pennsylvania State professional licensure. All EEES programs emphasize the value of integrative learning in the classroom, laboratory and field. Modern laboratories are well-equipped to support a wide range of courses and research experiences. Easy access to exceptional off-campus sites provides training in field methods that augment the curricula. A dedicated computer laboratory for geospatial technology (Geographic Information System, Global Positioning System, Remote Sensing) supports all EEES programs and research/project activities in the science and engineering fields. -
Growth and Erosion of Fold-And-Thrust Belts with an Application to the Aconcagua Fold-And-Thrust Belt, Argentina G
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 109, B01410, doi:10.1029/2002JB002282, 2004 Growth and erosion of fold-and-thrust belts with an application to the Aconcagua fold-and-thrust belt, Argentina G. E. Hilley1 and M. R. Strecker Institut fu¨r Geowissenschaften, Universita¨t Potsdam, Potsdam, Germany V. A. Ramos Department de Geologia, Universidad de Buenos Aires, Buenos Aires, Argentina Received 1 November 2002; revised 26 August 2003; accepted 11 September 2003; published 23 January 2004. [1] The development of topography within and erosional removal of material from an orogen exerts a primary control on its structure. We develop a model that describes the temporal development of a frontally accreting, critically growing Coulomb wedge whose topography is largely limited by bedrock fluvial incision. We present general results for arbitrary initial critical wedge geometries and investigate the temporal development of a critical wedge with no initial topography. Increasing rock erodibility and/or precipitation, decreasing mass flux accreting to the wedge front, increasing wedge sole-out depth, decreasing wedge and basal decollement overpressure, and increasing basal decollement friction lead to narrow wedges. Large power law exponent values cause the wedge geometry to quickly reach a condition in which all material accreted to the front of the wedge is removed by erosion. We apply our model to the Aconcagua fold-and-thrust belt in the central Andes of Argentina where wedge development over time is well constrained. We solve for the erosional coefficient K that is required to recreate the field-constrained wedge growth history, and these values are within the range of independently determined values in analogous rock types. -
Future Volcanism at Yellowstone Caldera: Insights from Geochemistry of Young Volcanic Units and Monitoring of Volcanic Unrest
2012 Annual Meeting & Exposition Issue! SEPTEMBER 2012 | VOL. 22, NO. 9 A PUBLICATION OF THE GEOLOGICAL SOCIETY OF AMERICA® Future volcanism at Yellowstone caldera: Insights from geochemistry of young volcanic units and monitoring of volcanic unrest Inside: Preliminary Announcement and Call for Papers: 2013 GSA Northeastern Section Meeting, p. 38 Preliminary Announcement and Call for Papers: 2013 GSA Southeastern Section Meeting, p. 41 VOLUME 22, NUMBER 9 | 2012 SEPTEMBER SCIENCE ARTICLE GSA TODAY (ISSN 1052-5173 USPS 0456-530) prints news and information for more than 25,000 GSA member read- ers and subscribing libraries, with 11 monthly issues (April/ May is a combined issue). GSA TODAY is published by The Geological Society of America® Inc. (GSA) with offices at 3300 Penrose Place, Boulder, Colorado, USA, and a mail- ing address of P.O. Box 9140, Boulder, CO 80301-9140, USA. 4 Future volcanism at Yellowstone GSA provides this and other forums for the presentation of diverse opinions and positions by scientists worldwide, caldera: Insights from geochemistry regardless of race, citizenship, gender, sexual orientation, of young volcanic units and religion, or political viewpoint. Opinions presented in this monitoring of volcanic unrest publication do not reflect official positions of the Society. Guillaume Girard and John Stix © 2012 The Geological Society of America Inc. All rights reserved. Copyright not claimed on content prepared Cover: View looking west into the Midway geyser wholly by U.S. government employees within the scope of basin of Yellowstone caldera (foreground) and the West their employment. Individual scientists are hereby granted permission, without fees or request to GSA, to use a single Yellowstone rhyolite lava flow (background). -
Geology, Geochemistry, and Geochronology of the Marigold Mine, Battle Mountain-Eureka Trend, Nevada
GEOLOGY, GEOCHEMISTRY, AND GEOCHRONOLOGY OF THE MARIGOLD MINE, BATTLE MOUNTAIN-EUREKA TREND, NEVADA by Matthew T. Fithian ! A thesis submitted to the Faculty and the Board of Trustees of the Colorado School of Mines in partial fulfillment of the requirements for the degree of Master of Science (Geology). Golden, Colorado Date ____________________ Signed: _______________________ Matthew T. Fithian Signed: _______________________ Dr. Elizabeth A. Holley Thesis Advisor Signed: _______________________ Dr. Nigel M. Kelly Thesis Co-Advisor Golden, Colorado Date ____________________ Signed: _______________________ Dr. Paul Santi Department Head Department of Geology and Geological Engineering ! ii! ABSTRACT The Marigold mine is located on the northern end of Nevada’s Battle Mountain-Eureka trend, approximately 55 km east-southeast of Winnemucca, Nevada in the Battle Mountain mining district. Marigold defines a N-S trending cluster of economic gold anomalies approximately 7 km long. Marigold has been historically described as a porphyry-related distal disseminated deposit based on the presence of porphyritic intrusions, proximity to known porphyry systems (e.g. Phoenix, Converse, Elder Creek), inferred high Ag:Au ratio, and limited understanding of sulfide mineralogy related to gold mineralization. The aim of this research was to examine the genesis of the gold mineralizing system at Marigold by determining the age of felsic porphyritic intrusions throughout the Marigold mine and the genetic relationship between these intrusions and gold mineralization. Geochronologic data were supplemented by geochemical sampling to understand the effect of the intrusions on the host rock, the effect of alteration on the intrusions, and the geochemical signature of gold ores. In addition to geochronologic and geochemical data, a secondary goal of the project was to determine the ore mineralogy below the redox boundary. -
The State Geological Surveys of the United States
DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, DIRECTOR BULLETIN 465 THE STATE GEOLOGICAL SURVEYS OF THE UNITED STATES COMPILED UNDER THE DIRECTION OF C. W. HAYES WASHINGTON GOVERNMENT PRINTING OFFICE 1911 CONTENTS. Page. Introduction.___________________._____________________ 5 Alabama___________________.__________________ 9 Arizona______________-._______________________ 10 Arkansas_______________________ _________.__________ 17 California___________________ ____________________ 20 Colorado__________'__..________________________ 24 Connecticut________________. ___________________ 29 Florida_____.._______ __ _________:.._____!_ 34 Georgia.._______ - 30 Illinois.-.-^-______________.-______________________ 42 Indiana______ _ _^=rr».- _--^ _ 51 Iowa__________________-____________________ 53 Kansas_____________ _ - _ _-__ 59 Maine__________________.- ___ __i_ __________ 63 Maryland______ _ ._-__ _ _ _____________ 69 Michigan_____ _ ___ _ 76 Minnesota__.._____________-____--- _ _______ SO Mississippi______..__ _--_ - __ 82 Missouri--________ _____ _- __ __ _ 86 Nebraska________ _ ,- __ 89 New Jersey_______ __ ___..- _ ..____ 90 New York____.__________-. ____________________:_ 98 North Carolina____________-__ _ __ __ ____ 101 North Dakota___-_._____J_.-___ -__ _ __ _________ 306 Ohio_____________________--__ ______________ 108 Oklahoma___________...--__- ___ _ ~- _ _ 116 Pennsylvania_______ _____________ _____ .__-__ ___ 122 Rhode Island___________________ __ _ __ 130 South Carolina__ -___ _______ _ 135 Tennessee-___ _______ ____ ___________ 138 Vermont____.._______._____. _ ..: __ 142 Virginia.- __ _ :__- 144 Washington_______ . - 149 West Virginia.. 153 Wisconsin___ -_ - 159 Appendix- 167 Internal Improvement Commission of Illinois__ ______________ 167 Territorial engineer of New Mexico __________ ___. 169 New York State Water Supply Commissiou 171 3 THE STATE GEOLOGICAL SURVEYS OF THE UNITED STATES. Compiled under the direction of C. W. HATES. -
Physical Stratigraphy and Facies Analysis of the Castissent Tecto-Sedimentary Unit (South-Central Pyrenees, Spain)
Miquel Poyatos-Moré PhD Dissertation Physical Stratigraphy and Facies Analysis of the Castissent Tecto-Sedimentary Unit (South-Central Pyrenees, Spain) Depositional processes and controlling factors of sediment dispersal from river-mouth to base-of-slope settings Universitat Autònoma de Barcelona February, 2014 Als meus pares, per empènye’m a no témer a res […] How many years can a mountain exist before it's washed to the sea? [...] (Dylan B., 1963, “Blowin' in the wind”) TABLE OF CONTENTS PREFACE AND ACKNOWLEDGEMENTS . 7 SUMMARY . 9 1. INTRODUCTION . 13 1.1. Overview 1.2. The shelf-to-slope transition: a key interphase 1.3. Fluvio-deltaic systems in active margins 1.4. Hyperpycnal-flow sedimentation 1.5. Channel-overbank complexes and slope turbidites 1.6. Sequence boundary recognition 1.7. Clinoforms and clinothems 1.8. Process regime vs Clinoform trajectory in passive margins 2. OBJECTIVES . 33 3. GEOLOGICAL SETTING AND PREVIOUS WORKS . 36 3.1. Structural framework of the study area 3.2. The lower Eocene depositional sequences 3.3. The Castissent Sequences 3.4. The Intra-Castissent sequence boundary 3.5. Chronostratigraphy of the Castissent Sequences 4. METHODOLOGY . 63 4.1. Geological Mapping 4.2. Logging of stratigraphic sections 4.3. Correlation panel 4.4. Facies description and analysis 4.5. Chronostratigraphy (magnetostratigraphy) 5. FACIES ANALYSIS OF THE CASTISSENT SEQUENCES . 78 5.1. Overview 5.2. Facies types 5.2.1. Gravel facies (G) 5.2.1.1. Clast supported conglomerates (Gcs) 5.2.1.2. Clast suported conglomerates grading into sandstones (CgS) 5.2.1.3. Sandy gravels (Gs) 5.2.1.4. -
Gneiss Domes and Gneiss Dome Systems
Geological Society of America Special Paper 380 2004 Gneiss domes and gneiss dome systems An Yin Department of Earth and Space Sciences and Institute of Geophysics and Planetary Physics, University of California, Los Angeles, California 90095-1567, USA ABSTRACT Various mechanisms have been proposed for the dynamic cause and kinematic development of gneiss domes. They include (1) diapiric fl ow induced by density inversion, (2) buckling under horizontal constriction (i.e., extension perpendicular to compression), (3) coeval orthogonal contraction or superposition of multiple phases of folding in different orientations, (4) instability induced by vertical variation of viscosity, (5) arching of corrugated detachment faults by extension-induced isostatic rebound, and (6) formation of doubly plunging antiforms induced by thrust-duplex development. Despite proliferation of models for gneiss-dome formation, a diagnos- tic link between the observed geological setting of a gneiss dome and the associated deformational processes remains poorly understood. This is because gneiss domes refl ect fi nite-strain patterns that can be reached through different strain paths or superposition of multiple mechanisms. To better differentiate the competing mechanisms and to assist the clarity of future discussion, a classifi cation scheme of individual gneiss domes and gneiss-dome systems is proposed. The scheme expands the traditional defi nition of mantled gneiss domes, which emphasizes the spatial association with synkinematic migmatite and a supracrustal cover, by including those associated with faults. To illustrate pos- sible kinematic interactions between faulting and gneiss-dome development, major geologic properties of two end-member fault-related gneiss domes are discussed: one produced by the development of North American Cordilleran-style extensional detachment faults and the other by passive-roof thrusts in crustal-scale fault-bend folds. -
This Report Is Preliminary and Has Not Been Reviewed for Conformity with the U.S
DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY NEW INFORMATION RESOURCES OF THE U.S. GEOLOGICAL SURVEY LIBRARY SYSTEM NUMBER 36 Apri1 1989 OPEN-FILE REPORT 89-400-D This report is preliminary and has not been reviewed for conformity with the U.S. Geological Survey editorial standards 1989 Main PAGE American mines handbook. Toronto : Northern Miner Press Ltd., / c!989- S(099) Am437 Geologic map of the Thatcher Mountain quadrangle, Box Elder County, Utah. Salt Lake City, Utah : Utah Geological and Mineral Survey, 1988. M(273)2 T324J Geologic map of the Black Hills area, South Dakota and Wyoming. Reston, Va. : U.S. Geological Survey, 1989. M(200) I no. 1910 Geological fieldwork 1988 : a summary of field activities and current research. Victoria, B.C. : Ministry of Energy, Mines and Petroleum Resources, [1989] 402(180) B777p no.1989-1 Mineral investigations resource map. Washington, D.C. : United States Geological Survey, 1952- M(200) MR Mineral resource assessment map of the Healy quadrangle, Alaska. Reston, Va. : U.S. Geological Survey, 1989. M(200) MF no.2058-A Mineral resources of the central part of the Independence mining district, Park and Sweet Grass Counties, Montana / by Phillip R. Moyle ... [et al.]. Spokane, Wash. : Western Field Operations Center, U.S. Dept. of the Interior, Bureau of Mines, [1989] 402(200) Un34msi no.89-4 Mining in Ecuador. Quito : The Institute. 420(465) qM664 Road log of the Chatham, Randolph and Orange County areas, North Carolina : annual meeting, Carolina Geological Society, November 7-8, 1964. Raleigh : The Society, [1964] G(231) qC22g 1964 SMSS technical monograph. -
U.S. DEPARTMENT of the INTERIOR U.S.GEOLOGICAL SURVEY ALK.BIB a Selected Bibliography of Alkaline Igneous Rocks and Related Mine
U.S. DEPARTMENT OF THE INTERIOR U.S.GEOLOGICAL SURVEY ALK.BIB A selected bibliography of alkaline igneous rocks and related mineral deposits, with an emphasis on western North America compiled by Felix E. Mutschler, D. Chad Johnson, and Thomas C. Mooney Open-File Report 94-624 1994 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. INTRODUCTION This bibliography contains 3,406 references on alkaline igneous rocks and related mineral deposits compiled in conjunction with ongoing studies of alkaline igneous rocks, metallogeny, and tectonics in western North America. Much of the literature on these topics is not readily recovered by searches of current bibliographies and computerized reference systems. We hope that by making this bibliography available, it will help other workers to access this occasionally hard to find literature. The bibliography is available in two formats: (1) paper hardcopy and (2) Apple Macintosh computer-readable 3.5 inch double density diskette. The computer-readable version of the bibliography is a 725 KB WORD (version 5.0) document. Individual literature citations are arranged alphabetically by author(s) and the order of items in each citation follows the standard U.S. Geological Survey format. Version 3.4 1 February 1994 BIBLIOGRAPHY Abbott, J. G., Gordey, S. P., and Tempelman-Kluit, D. J., 1986, Setting of stratiform, sediment- hosted lead-zinc deposits in Yukon and northeastern British Columbia, in Morin, J. -
Structural Systems and Paragenetic Assemblages At
Manuscript Click here to download Manuscript: Veloso et al - Main text.docx 1 Structural Systems and Paragenetic Assemblages at 2 the Dominga Fe-Cu Deposit: Tectono-Metallogenic 3 Evolution 4 5 Veloso, E.1 (corresponding author), Email: [email protected] 6 Cembrano, J.2, Email: [email protected] 7 Arancibia, G.2, Email: [email protected] 8 Heuser, G.2, Email: [email protected] 9 Neira, S.3, Email: [email protected] 10 Siña, A.3, Email: [email protected] 11 Garrido, I.3, Email: [email protected] 12 Vermeesch, P.4, Email: [email protected] 13 Selby, D. 5, Email: [email protected] 14 Santibáñez, I.2, Email: [email protected] 15 Pérez-Flores, P.2, Email: [email protected] 16 Gomila, R.2, Email: [email protected] 17 18 1 Fundación Norte Sustentable, Avenida Cerro El Plomo 5460, Piso 19, Las Condes, Santiago, Chile. 19 2 Departamento de Ingeniería Estructural y Geotécnica, Pontificia Universidad Católica de Chile, Avenida 20 Vicuña Mackenna 4860, Macul, Santiago, Chile. 21 3 Andes Iron SpA, Avenida Cerro El Plomo 5460, Piso 19, Las Condes, Santiago, Chile. 22 4 Department of Earth Sciences, University College London, Gower Street, London WC1E 6BT, UK. 23 5 Department of Earth Sciences, University of Durham, Durham DH1 3LE, UK. 24 25 1 26 Abstract 27 The Dominga district, northern Chile, shows a spatial and genetic affinity among distinctive 28 structural elements and occurrence of Fe-Cu-rich paragenetic mineral assemblages. Deep seated, NE-to- 29 EW striking structural elements form a right-lateral duplex-like structural system (Early Structural 30 System, ESS) that cut regionally altered (stage I) rocks.