Genesis and Geochronology of Alkaline Volcanism in the Pinacate Volcanic Field Northwestern Sonora, Mexico

Total Page:16

File Type:pdf, Size:1020Kb

Genesis and Geochronology of Alkaline Volcanism in the Pinacate Volcanic Field Northwestern Sonora, Mexico Genesis and geochronology of alkaline volcanism in the Pinacate Volcanic Field Northwestern Sonora, Mexico Item Type text; Dissertation-Reproduction (electronic) Authors Lynch, Daniel James, 1940- Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 10/10/2021 04:47:41 Link to Item http://hdl.handle.net/10150/565497 GENESIS AND GEOCHRONOLOGY OF ALKALINE VOLCANISM IN THE PINACATE VOLCANIC FIELD NORTHWESTERN SONORA, MEXICO by Daniel James Lynch II A Dissertation Submitted to the Faculty of the Department of Geosciences ,In Partial Fulfillment of the Requirements For the Degree of DOCTOR OF PHILOSOPHY In the Graduate College THE UNIVERSITY OF ARIZONA 19 8 1 THE UNIVERSITY OF ARIZONA GRADUATE COLLEGE As members of the Final Examination Committee, we certify that we have read the dissertation prepared by ____Daniel James Lynch II______________________ entitled Genesis and Geochronology of Alkaline Volcanism in the Pinacate Volcanic Field, Northwestern Sonora, Mexico and recommend that it be accepted as fulfilling the dissertation requirement for the Degree of Doctor of Philosophy C P f c . / r / 9 f / Date Dfc. [?, Date — UA * D f c IT, Date Date Date Final approval and acceptance of this dissertation is contingent upon the candidate's submission of the final copy of the dissertation to the Graduate College. I hereby certify that I have read this dissertation prepared under my direction and recommend that it be accepted as fulfilling the dissertation requirement. Dissertation Director STATEMENT BY AUTHOR This dissertation has been submitted in partial fulfillment of requirements for an advanced degree at The University of Arizona and is deposited in the University Library to be made available to borrowers under rules of the Library. Brief quotations from this dissertation are allowable without special permission, provided that accurate acknowledgement of source is made. Requests for permission for extended quotation from or re­ production of this manuscript in whole or in part may be granted by the head of the major department or the Dean of the Graduate College when in his judgement the proposed use of the material is in the interests of scholarship. In all other instances, however, permission must be obtained from the author. SIGNED! /1. *i ; Cs ACKNOWLEDGEMENTS The work was done while I was employed in the Laboratory of Isotope Geochemistry in the Department of Geosciences at the University of Arizona. Support was furnished by the National Science Foundation under Grant Number EAR-78-11535, Paul E. Damon, Principal Investigator. Additional support was provided by the State of Arizona and by the Consejo Naturales no Removables of the government of Mexico. I especially wish to thank Dr. Paul Damon for his support and supervision of this dissertation. Not only this work, but my general education benefitted from long discussions with Drs. Mohammed Shafiqullah, William B. Bull and George H. Davis. The manuscript was improved with suggestions from Dr. Charles A. Wood, NASA Houston, and Peter Kresan of the University of Arizona, made in addition to those of my committee members. During the course of my field investigations, I shamelessly pressed my wife, Elaine, and my friends John Proids, Hugh Warren and Dave Dennis into service as sherpas to lug rocks down the mountain. A1 and Juanita Healey flew me on two photographic missions around the field. Song-Lin Cheng aided with the chemical and strontium analyses. Robert Bucher, quintessential jack of all trades, did the glass blowing for argon analyses and lettered my illustrations. My thanks to the numerous denizens of the mineral separation laboratory, now long vanished, who worked at sample preparation. ' Finally, I offer my profoundest gratitude to MFD for leaving Santa Clara for me. TABLE OF CONTENTS Page LIST OF ILLUSTRATIONS....................................... vii LIST OF TABLES................................................ ABSTRACT........... xi 1. INTRODUCTION - THE VOLCANIC FIELD AND ITS SETTING............. 1 Purpose and Scope................... Geography and History of Exploration. Location and Climate............ Early Inhabitants and Exploration Previous Geologic Investigation.. Geology of the Finacate Region...... L«J Ul Ui OX 00 VO Geologic Evolution of the Region......... 11 Contemporaneous Volcanic Fields...................... 12 Development of the Gulf of California.......... 15 Site Geology........................... .17 The Country Rocks............ 20 The Landscape and Ephemeral Water........... ...24 Sand of the Gran Desierto............................ 27 2. THE PINACATE VOLCANOES....................................... 30 Structural Features of the Volcanic Field............ ....34 Cone Alignments...................................... 34 Relationships of Faulting and Volcanism..............37 Effects of Gulf of California Tectonism............. 42 The Pinacate Series Lavas................................ 43 Petrography.......................................... 45 Geochemistry......................................... 49 Strontium Isotope Ratios......................... 51 Geochronology of the Pinacate Volcanism..............53 Pinacate Volcanic Features............................... 57 Lava Flows........................................... 57 Cinder and Agglutinate Cones....................... .58 Histories of Two Typical Pinacate Volcanoes..........65 Carnegie Cone.................................... 65 Tecolote Cone.................. ...67 Other Noteworthy Features....... 76 Hilltop Volcanoes................................ 76 The "Pit" Crater................. 76 iv V TABLE OF CONTENTS — Continued Page 3. THE GREAT MAAR CRATERS.............................. 80 Descriptions and Scenarios................................... 84 Elegante Crater.......................................... 84 MacDougal and Molina Craters............................. 91 Sykes Crater..... ................ ................ .......95 Cerro Colorado Crater.................................... 97 Crater Elena Tuff Cone......... 100 Moon Crater............................................. 101 The Other Hydro-Volcanic Features...................... 103 A Hydrovolcanic Model....................................... 103 4. VOLCAN SANTA CLARA.......................................... 112 Nature and Implications of the Alkaline Rock Series...... 118 The Santa Clara Volcanic Series......................... 120 Distribution of the Lavas.......................... .120 Geochronology...................................... 123 Character of the Rock.............................. 125 Petrography............... ......................... 126 The Nodules......................................... 127 Geochemistry............................. .......... 129 Major Elements............. .................. .129 Trace Elements .......... ........................ 136 Strontium Isotopes........ ..................... 145 Benmoreite "B", the Compositional Reversal........... 145 Summary..................................................148 Similar Alkaline Volcanic Fields........................ 148 5. ORIGINS OF PINACATE AND SANTA CLARA - A GENERAL MODEL........ 152 The Nature and Source of the Alkali- Olivine-Basalt Magma Type...........152 Origin of the Pinacate and Santa Clara Magma Bodies...... 159 A General Volcanic Model ....... ................. 162 vi TABLE OF CONTENTS — Continued Page APPENDIX I: GEOGRAPHY AND ACCESS........................... 170 Worldwide Volcano Locator........................ *......170 Maps and Photographic Coverage.......................... 171 Access......... .........................................172 APPENDIX II: EXPERIMENTAL TECHNIQUES....................... 173 Sample Collection and Preparation....................... 173 "Whole Rock" Age Determination.......................... 173 Strontium Isotope Analysis....... 175 Whole Rock Chemistry.....................................177 APPENDIX III: SAMPLE DATA.................................. 179 REFERENCES CITED 233 LIST OF ILLUSTRATIONS Figure Page 1. VOLCAN SANTA CLARA AND THE PINACATE VOLCANOES............. 2 2. GEOLOGIC PROVINCES SURROUNDING THE PINACATE REGION........ 10 3. LATE NEOCENE VOLCANIC FIELDS OF THE PINACATE REGION....... 13 4. LANDSAT/ERTS VIEW.......................................... 18 5. GEOLOGIC PHOTOGRAPH OF THE PINACATE AREA.................. 21 6. RIO DE SONOYTA AT BATAMOTE............................... ..25 7. SAND PATTERNS AROUND PYRAMID CONE (CC 5940)............ ....28 8. SKYLAB 4 PHOTOGRAPH OF THE PINACATE AREA...................31 9. CONES OF THE SOUTH FLANK................................... 32 10. STRUCTURAL FEATURES MAP.................................... 35 11. STRUCTURAL ROSE DIAGRAM.................................... 36 12. STRESS REGIMES OF FAULTING AND MAGMA INTRUSION.............39 13. COMPOSITIONAL FIELDS OF THE ALKALINE ROCKS..... ........... 44 14. BARKER DIAGRAMS OF THE PINACATE SERIES ROCKS...............50 15. LOCATIONS OF DATED SAMPLES................................. 55 16. PHILLIPS BUTTES............................................ 62 17. CARNEGIE CONE ON THE SUMMIT PLATFORM....................... 64 18. SPATTER CONES.............................................. 66 19. PAHOEHOE SPATTER
Recommended publications
  • On Celestial Wings / Edgar D
    Library of Congress Cataloging-in-Publication Data Whitcomb. Edgar D. On Celestial Wings / Edgar D. Whitcomb. p. cm. Includes bibliographical references. 1. United States. Army Air Forces-History-World War, 1939-1945. 2. Flight navigators- United States-Biography. 3. World War, 1939-1945-Campaigns-Pacific Area. 4. World War, 1939-1945-Personal narratives, American. I. Title. D790.W415 1996 940.54’4973-dc20 95-43048 CIP ISBN 1-58566-003-5 First Printing November 1995 Second Printing June 1998 Third Printing December 1999 Fourth Printing May 2000 Fifth Printing August 2001 Disclaimer This publication was produced in the Department of Defense school environment in the interest of academic freedom and the advancement of national defense-related concepts. The views expressed in this publication are those of the author and do not reflect the official policy or position of the Department of Defense or the United States government. This publication has been reviewed by security and policy review authorities and is cleared for public release. Digitize February 2003 from August 2001 Fifth Printing NOTE: Pagination changed. ii This book is dedicated to Charlie Contents Page Disclaimer........................................................................................................................... ii Foreword............................................................................................................................ vi About the author ..............................................................................................................
    [Show full text]
  • Comments On'kaersutite from San Carlos, Arizona, with Comments On
    MINERALOGICAL MAGAZINE, SEPTEMBER I969, VOL. 37, NO. 287 Comments on 'Kaersutite from San Carlos, Arizona, with comments on the paragenesis of this mineral' by Brian Mason MARTIN PRINZ ~ Department of Geology, University of New Mexico, Albuquerque, New Mexico 87Io6 AND C. E. NEHRU Department of Geology, Brooklyn College, Brooklyn, New York II2~O s u MM A R Y. Electron probe analyses have been made of eight kaersutites from San Carlos, A~cizona, and one from Kakanui, New Zealand; also of olivine, clinopyroxene, ilmenite, and spinel from San Carlos. There is not as yet adequate evidence that the kaersutite is an upper mantle phase. MASON (I968a) suggests that kaersutite, as exemplified by the occurrence at San Carlos, Arizona, as well as from some other localities, may represent the amphibole phase in upper mantle rocks. The possibility of amphibole as an upper mantle phase was most clearly suggested by Oxburgh (I964) since it would help explain the alkali content of basaltic rocks, which otherwise would be derived from alkali-poor ultra- mafic mantle rocks. Since we are carrying out a detailed study of the ultramafic inclusions of the San Carlos, Arizona, locality, we would like to clarify some of the petrologic significance of the kaersutite from this area because it leads us to different conclusions from those of Mason. Hopefully, our comments will be of value to others suggesting amphibole as an upper mantle phase. San Carlos locality. The kaersutite described by Mason (I968a) in the San Carlos locality occurs as a granular aggregate of anhedral crystals, with a little inter-granular ilmenite.
    [Show full text]
  • Summary of the Mineral Information Package for the Khanneshin Carbonatite Area of Interest
    Chapter 21A. Summary of the Mineral Information Package for the Khanneshin Carbonatite Area of Interest Contribution by Robert D. Tucker, Harvey E. Belkin, Klaus J. Schulz, Stephen G. Peters, and Kim P. Buttleman Abstract The Khanneshin carbonatite is a deeply dissected igneous complex of Quaternary age that rises approximately 700 meters above the flat-lying Neogene sediments of the Registan Desert, Helmand Province, Afghanistan. The complex consists almost exclusively of carbonate-rich intrusive and extrusive igneous rocks, crudely circular in outline, with only three small hypabyssal plugs of leucite phonolite and leucitite outcropping in the southeastern part of the complex. The complex is broadly divisible into a central intrusive vent (or massif), approximately 4 kilometers in diameter, consisting of coarse-grained sövite and brecciated and agglomeratic barite-ankerite alvikite; a thin marginal zone (less than 1 kilometer wide) of outwardly dipping (5°–45°). Neogene sedimentary strata; and a peripheral apron of volcanic and volcaniclastic strata extending another 3–5 kilometers away from the central intrusive massif. Small satellitic intrusions of biotite-calcite carbonatite, no larger than 400 meters in diameter, crop out on the southern and southeastern margin of the central intrusive massif. In the 1970s several teams of Soviet geologists identified prospective areas of interest for uranium, phosphorus, and light rare earth element (LREE) mineralization in four regions of the carbonatite complex. High uranium concentrations are reported in two regions; the greatest concentrations are confined to silicified shear zones in sandy clay approximately 1.1 kilometers southwest of the peripheral part of the central vent. An area of phosphorus enrichment, primarily occurring in apatite, is present in coarse-grained agglomeratic alvikite, with abundant fenite xenoliths, approximately 750 meters south of the periphery of the central vent.
    [Show full text]
  • Charles Darwin: a Companion
    CHARLES DARWIN: A COMPANION Charles Darwin aged 59. Reproduction of a photograph by Julia Margaret Cameron, original 13 x 10 inches, taken at Dumbola Lodge, Freshwater, Isle of Wight in July 1869. The original print is signed and authenticated by Mrs Cameron and also signed by Darwin. It bears Colnaghi's blind embossed registration. [page 3] CHARLES DARWIN A Companion by R. B. FREEMAN Department of Zoology University College London DAWSON [page 4] First published in 1978 © R. B. Freeman 1978 All rights reserved. No part of this publication may be reproduced, stored in a retrieval system, or transmitted, in any form or by any means, electronic, mechanical, photocopying, recording or otherwise without the permission of the publisher: Wm Dawson & Sons Ltd, Cannon House Folkestone, Kent, England Archon Books, The Shoe String Press, Inc 995 Sherman Avenue, Hamden, Connecticut 06514 USA British Library Cataloguing in Publication Data Freeman, Richard Broke. Charles Darwin. 1. Darwin, Charles – Dictionaries, indexes, etc. 575′. 0092′4 QH31. D2 ISBN 0–7129–0901–X Archon ISBN 0–208–01739–9 LC 78–40928 Filmset in 11/12 pt Bembo Printed and bound in Great Britain by W & J Mackay Limited, Chatham [page 5] CONTENTS List of Illustrations 6 Introduction 7 Acknowledgements 10 Abbreviations 11 Text 17–309 [page 6] LIST OF ILLUSTRATIONS Charles Darwin aged 59 Frontispiece From a photograph by Julia Margaret Cameron Skeleton Pedigree of Charles Robert Darwin 66 Pedigree to show Charles Robert Darwin's Relationship to his Wife Emma 67 Wedgwood Pedigree of Robert Darwin's Children and Grandchildren 68 Arms and Crest of Robert Waring Darwin 69 Research Notes on Insectivorous Plants 1860 90 Charles Darwin's Full Signature 91 [page 7] INTRODUCTION THIS Companion is about Charles Darwin the man: it is not about evolution by natural selection, nor is it about any other of his theoretical or experimental work.
    [Show full text]
  • Geology of the Nairobi Region, Kenya
    % % % % % % % % %% %% %% %% %% %% %% % GEOLOGIC HISTORY % %% %% % % Legend %% %% %% %% %% %% %% % % % % % % HOLOCENE: %% % Pl-mv Pka %%% Sediments Mt Margaret U. Kerichwa Tuffs % % % % %% %% % Longonot (0.2 - 400 ka): trachyte stratovolcano and associated deposits. Materials exposed in this map % %% %% %% %% %% %% % section are comprised of the Longonot Ash Member (3.3 ka) and Lower Trachyte (5.6-3.3 ka). The % Pka' % % % % % % L. Kerichwa Tuff % % % % % % Alluvial fan Pleistocene: Calabrian % % % % % % % Geo% lo% gy of the Nairobi Region, Kenya % trachyte lavas were related to cone building, and the airfall tuffs were produced by summit crater formation % % % % % % % % % % % % % % % % % Pna % % % % %% % (Clarke et al. 1990). % % % % % % Pl-tb % % Narok Agglomerate % % % % % Kedong Lake Sediments Tepesi Basalt % % % % % % % % % % % % % % % % %% % % % 37.0 °E % % % % 36.5 °E % % % % For area to North see: Geology of the Kijabe Area, KGS Report 67 %% % % % Pnt %% % PLEISTOCENE: % % %% % % % Pl-kl %% % % Nairobi Trachyte % %% % -1.0 ° % % % % -1.0 ° Lacustrine Sediments % % % % % % % % Pleistocene: Gelasian % % % % % Kedong Valley Tuff (20-40 ka): trachytic ignimbrites and associated fall deposits created by caldera % 0 % 1800 % % ? % % % 0 0 % % % 0 % % % % % 0 % 0 8 % % % % % 4 % 4 Pkt % formation at Longonot. There are at least 5 ignimbrite units, each with a red-brown weathered top. In 1 % % % % 2 % 2 % % Kiambu Trachyte % Pl-lv % % % % % % % % % % %% % % Limuru Pantellerite % % % % some regions the pyroclastic glass and pumice has been
    [Show full text]
  • The Mineralogy and Chemistry of the Anorogenic Tertiary Silicic Volcanics
    JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 86, NO. Bll, PAGES 10242-10256, NOVEMBER 10, 1981 The Mineralogyand Chemistryof the AnorogenicTertiary SilicicVolcanics of S.E. Queenslandand N.E. New South Wales, Australia A. EWART Departmentof Geology& Mineralogy,University of Queensland,St. Lucia,Brisbane, Queensland 4067 The Late Oligocene-EarlyMiocene volcanismof this regionis chemicallystrongly bimodal; the mafic lavas(volmetrically dominant) comprise basalts, hawaiites, and tholeiiticandesites, while the silicic eruptivesare mainly comendites,potassic trachytes, and potassic,high-silica rhyolites.The comendites and rhyoliteshave distinctivetrace element abundancepatterns, notably the extreme depletionsof Sr, Ba, Mg, Mn, P, Cr, V, and Eu, and the variable em'ichraentof suchelements as Rb, Zr, Pb, Nb, Zn, U, and Th. The trachytesexhibit thesecharacteristics to lesserdegrees. The comenditesare distinguished from the rhyolitesby their overall relative enrichmentof the more highly chargedcations (e.g., LREE, Nb, Y, and especiallyZr) and Zn. The phenocrystmineralogy of the trachytesand rhyolitescomprises various combinationsof the following phases:sodic plagioclase(albite-andesine), calcic anorthoclase, sanidine, quartz, ferroaugite-ferrohedenbergite,ferrohypersthene, fayalitic olivine, ilmenite, titano- magnetite,and rarely biotite (near annite) and Fe-hastingsiticamphibole. Accessories include apatite, zircon, chevkinite (ferrohedenbergite-bearingrhyolites only), and allanite (amphibole and botite rhyo- lites only). The comenditesgenerally contain
    [Show full text]
  • Source to Surface Model of Monogenetic Volcanism: a Critical Review
    Downloaded from http://sp.lyellcollection.org/ by guest on September 28, 2021 Source to surface model of monogenetic volcanism: a critical review I. E. M. SMITH1 &K.NE´ METH2* 1School of Environment, University of Auckland, Auckland, New Zealand 2Volcanic Risk Solutions, Massey University, Palmerston North 4442, New Zealand *Correspondence: [email protected] Abstract: Small-scale volcanic systems are the most widespread type of volcanism on Earth and occur in all of the main tectonic settings. Most commonly, these systems erupt basaltic magmas within a wide compositional range from strongly silica undersaturated to saturated and oversatu- rated; less commonly, the spectrum includes more siliceous compositions. Small-scale volcanic systems are commonly monogenetic in the sense that they are represented at the Earth’s surface by fields of small volcanoes, each the product of a temporally restricted eruption of a composition- ally distinct batch of magma, and this is in contrast to polygenetic systems characterized by rela- tively large edifices built by multiple eruptions over longer periods of time involving magmas with diverse origins. Eruption styles of small-scale volcanoes range from pyroclastic to effusive, and are strongly controlled by the relative influence of the characteristics of the magmatic system and the surface environment. Gold Open Access: This article is published under the terms of the CC-BY 3.0 license. Small-scale basaltic magmatic systems characteris- hazards associated with eruptions, and this is tically occur at the Earth’s surface as fields of small particularly true where volcanic fields are in close monogenetic volcanoes. These volcanoes are the proximity to population centres.
    [Show full text]
  • February 2014
    STATE GAZETTE I SUNDAY FEBRUAFY 2,2014 THE JACKSON SUN . SUNDAY,FEB.2,2014 UTM Ripley Center offers Internet UT Martin mu$Gum basics course The University of Ten- Gommemorates nessee Martin Office of exhibit Extended Campus and Online Studies is sponsor- ing an Internet basics 50th anniYcrsary of course. The course will be offered from 1, to 4 p.m. Thursday at the UT Tennessee sit-ins Martin Ripley Center. Tangelia Fayne-Yar- Special to the State Gazette bough will teach the MARTIN Tenn. - An intimate look at the role course, according-to a Tbnnessee students played in shaping the modern news reiease. The course Civil Rights Movement is explored in "We Shall Not is an opportunity to learn Be Moved: The 50th Anniversary of Tennessee's Civil how to navigate through Rights Sit-Ins" - an exhibit featured at the J. Houston the Internet, create an Gordon Museum at the University of Tennessee at email account, use Inter- Martin. net etiquette in sending fire exhibit, on display from Feb. l-March 14, fea- emails, attach documents tures artifacts, photographic images, and audiovisual to an email message, in- media related to the nonviolent direct-action cam- corporate text in the body of an email, create pargn to end racial segregation at lunch counters in folders for individual downtown Nashville which occurred from Feb. 13 to documents, store impor- May 10, 1960. tant documents for fu- Fifty years ago, a handfirl of Nashville college stu- ture use and delete items dents from Fisk University Tennessee A&I (later that are no longer need- Tennessee State) and American Baptist Theological ed.
    [Show full text]
  • Module 7 Igneous Rocks IGNEOUS ROCKS
    Module 7 Igneous Rocks IGNEOUS ROCKS ▪ Igneous Rocks form by crystallization of molten rock material IGNEOUS ROCKS ▪ Igneous Rocks form by crystallization of molten rock material ▪ Molten rock material below Earth’s surface is called magma ▪ Molten rock material erupted above Earth’s surface is called lava ▪ The name changes because the composition of the molten material changes as it is erupted due to escape of volatile gases Rocks Cycle Consolidation Crystallization Rock Forming Minerals 1200ºC Olivine High Ca-rich Pyroxene Ca-Na-rich Amphibole Intermediate Na-Ca-rich Continuous branch Continuous Discontinuous branch Discontinuous Biotite Na-rich Plagioclase feldspar of liquid increases liquid of 2 Temperature decreases Temperature SiO Low K-feldspar Muscovite Quartz 700ºC BOWEN’S REACTION SERIES Rock Forming Minerals Olivine Ca-rich Pyroxene Ca-Na-rich Amphibole Na-Ca-rich Continuous branch Continuous Discontinuous branch Discontinuous Biotite Na-rich Plagioclase feldspar K-feldspar Muscovite Quartz BOWEN’S REACTION SERIES Rock Forming Minerals High Temperature Mineral Suite Olivine • Isolated Tetrahedra Structure • Iron, magnesium, silicon, oxygen • Bowen’s Discontinuous Series Augite • Single Chain Structure (Pyroxene) • Iron, magnesium, calcium, silicon, aluminium, oxygen • Bowen’s Discontinuos Series Calcium Feldspar • Framework Silicate Structure (Plagioclase) • Calcium, silicon, aluminium, oxygen • Bowen’s Continuous Series Rock Forming Minerals Intermediate Temperature Mineral Suite Hornblende • Double Chain Structure (Amphibole)
    [Show full text]
  • Kaersutite-Bearing Xenoliths and Megacrysts in Volcanic Rocks from the Funk Seamount in the Southwest Indian Ocean
    Kaersutite-bearing xenoliths and megacrysts in volcanic rocks from the Funk Seamount in the southwest Indian Ocean ARCH M. REID* AND ANTON P. LE ROEX Department of Geology, University of Cape Town, Rondebosch 7700, South Africa Abstract Eight samples (seven volcanic rocks and one quartz sandstone) have been dredged from the Funk Seamount, 60 km NW of Marion Island in the southwest Indian Ocean Oat. 46 ~ 15' S, long. 37 ~ 20' E). The volcanic rocks are fine-grained vesicular basanitoids and glass-rich volcanic breccias geochemically similar to the Marion Island lavas. Lavas and breccias contain a suite of megacryst minerals and of small polymineralic xenoliths, in both of which kaersutite is a prominent constituent. The megacryst suite comprises large unzoned single grains of kaersutite, plagioclase, pyroxene, magnetite and ilmenite, all showing textural evidence of resorption/reaction with the basanitoid host. The megacrysts have a limited range of compositions except for the plagioclase which ranges from oligoclase to labradorite. The small (2 mm to ~ 3 cm) xenoliths are mostly two-pyroxene amphibole assemblages with or without olivine, magnetite, ilmenite, plagioclase and apatite. The xenoliths show some evidence of reaction with the basanitoid host and most have undergone recrystallization and/or localised decompression melting. Xenolith and megacryst assemblages are interpreted as being associated with the formation and partial crystallization of a hydrous basanitoid melt at depth. KEYWORDS: kaersutite, amphibole, xenolith, Funk Seamount, Indian Ocean. Introduction megacrysts. Brown amphibole is a prominent con- stituent of both xenolith and megacryst suites. F U N K S E A M O U N T is a prominent seamount situa- Mantle xenoliths in abyssal lavas are rare and so ted 60 km to the NW of Marion and Prince Edward these samples are of particular interest.
    [Show full text]
  • A Unique Volcanic Field in Tharsis, Mars: Monogenetic Cinder Cones and Lava Flows As Evidence for Hawaiian Eruptions
    42nd Lunar and Planetary Science Conference (2011) 1379.pdf A UNIQUE VOLCANIC FIELD IN THARSIS, MARS: MONOGENETIC CINDER CONES AND LAVA FLOWS AS EVIDENCE FOR HAWAIIAN ERUPTIONS. P. Brož1 and E. Hauber2, 1Institute of Geophysics ASCR, v.v.i., Prague, Czech Republic, [email protected], 2Institut für Planetenforschung, DLR, Berlin, Germany, [email protected]. Introduction: Most volcanoes on Mars that have Data: We use images from several cameras, i.e. been studied so far seem to be basaltic shield volca- Context Camera (CTX), High Resolution Stereo Cam- noes, which can be very large with diameters of hun- era (HRSC), and High Resolution Imaging Science dreds of kilometers [e.g., 1] or much smaller with di- Experiment (HiRISE) for morphological analyses. ameters of several kilometers only [2]. Few Viking Topographic information (e.g., heights and slope an- Orbiter-based studies reported the possible existence gles) were determined from single shots of the Mars of cinder cones [3,4] or stratovolcanoes [5-7], and only Orbiter Laser Altimeter (MOLA) in a GIS environ- the advent of higher-resolution data led to the tentative ment, and from stereo images (HRSC, CTX) and de- interpretation of previously unknown edifices as cinder rived gridded digital elevation models (DEM). cones [8] or rootless cones [9]. The identification of Morphometry: For comparison between the cinder cones can constrain the nature of eruption proc- cones and terrestrial morphological analogues (i.e. esses and, indirectly, our understanding of the nature cinder cones [10]) we determined some basic mor- of parent magmas (e.g., volatile content). Here we re- phometric properties and their ratios (e.g., crater di- port on our observation of a unique cluster of possible ameter [WCR] vs.
    [Show full text]
  • 31 a Preliminary Study Of
    31 A PRELIMINARY STUDY OF THE: TERTIARY VOLCANIC AND SEDIMENTARY ROCKS, GÜMELE, ESKİŞEHİR Eskişehir, Gümele Çevresindeki Tersiyer Volkanik ve Sedimanter Kayaçlarda Bir Ön Çalışma Taylan Lünel Middle East Technical University, Department of Geological Engineering Ankara ÖZ. — Seyitgazi-Eskişehir antiklinoriumu'nun çok fazla deforme olmuş ve metamorfizmaya uğramış kayaçlarının kuzey-kuzeybatısında bulunan sedimanter ve volkanik kayaçlar incelenmiştir. Karasal ve gölsel fasiyesde meydana gelen Tersi- yer sedimanter kayaçlar Güney Eskişehir küvetinde olunmuşlardır. Karasal fasiye- si meydana getiren kayaç birimlerini kaba kumtaşları, kumtaşları, bitki kalıntıları ihtiva eden kil ve marnlar ve serpantinit blokları taşıyan bazal konglomerası teşkil etmektedir. Gölsel fasiyes ise genellikle killi ve tüflü kalkerler, kalkerler, marnlar, kon- glomeralar ve tüflerden meydana gelmiştir. Küvetteki en eski sedimanlar ve piroklas- tikler Alt Miosen'de oluşmuşlardır. Yataya yakın konumlanmış bazik-intermediyar lav akıntıları Pliosen yaşlı olup Altüst Neojen sedimantasyon kesikliğinde meyda- na gelmiştir. Üst Neojen sedimanter kayaçları intermediyar-basaltik volkaniklerin üzerinde ince bandlar şeklinde bulunurlar. Bu birim marn ve kalkerlerden meyda- na gelmiştir. Alt Miosen’de asid volkanik faaliyetler neticesinde meydana gelen sil- lar (unweldd tuffs) oligomikt konglomeralardan evvel teşekkül etmiştir. Bu volkanik aktitivite muhtemelen kesikli ve kısıtlı olarak devam etmiş ve tüflü kalkerleri mey- dana getirmiştir. Pliosen yaşlı bazik-intermediyar
    [Show full text]