LAVAS of HA Wail and THEIR RELATIONS·

Total Page:16

File Type:pdf, Size:1020Kb

LAVAS of HA Wail and THEIR RELATIONS· DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMrL'J:I, DIRECTOR '· PROFESSIONAL PAPER 88 LAVAS OF HA_ WAil AND THEIR RELATIONS· BY WHITMAN CllOSS WASHINGTON GOVERNMENT PRINTING OFFICE 1915 • CONTENTS. Page. Introduction ......................................... , .. _, ................................... : .......... 7 Publications cited ..................... ·_ .............................................................. _. ... 8 Petrography ....................................... _... ____ . ________ .. _.... __________ .. _____ ...... _____ ... 9 ~'he lesser islands ................................................................................... 9 Island of ](u.uai .................................................................................... 9 bccu.rrence and sources of material studied ...............................· ........................ 9 Olivine-plu.gioclase basalt ....................................................................... 10 Genet·al characters.~ ............................ -.- ............... : .......................... 10 Chemical composition ....................................................................... 10 Quu.ntitative classification .................................................................. 12 Helation of norm and mode in rocks analyzed ................................................ 12 Plu.gioclase basalt (poor in olivine) .......................· ......................................... 13 ]~itnburgite .......................... ~ ........ -... -..... ------------ .. -.-.--- ·----- -.-------- ·--- 13 Oligoclase gabbro or kauaiite ..................................................................... .. 14 Occurrence .............................. -·- .................................................. 14 ])escription .......................... _.... _. ____ . _............. _. _. ___ . _... _... _... ______ ... 14 Chemical composition ........ : ................................................................ 15 Quantitative classification ................................................................... 15 Systematic relations and name kauaiite ............- .......................................... 16 Melilite-nephelite basalt ........................................................................ 16 Occurrence ................................................................................. 16 Description ...................................................... _____ ... __ .................. 16 Chenlical con1position ........................................................................ 16 Quantitative classification ................................................................... 17 Basalts des·cribed by Mohle ...................................................................... 17 Island of Oahu ........................................................................................ 17 -. Introductory note .............................................· .................................... 17 T Hange of lavas ............................ __ .............· ............................... __ ._._ .. 18 Olivine-plagioclase basalt ............................ ·- ........................................... 18 Bronzite-bearing basalt ........................................................................... 19 Plagioclase basalt (olivine free) .................· ...........· ...................................... 20 Nephelite-melilite basalt ................................................... ·...... ·.· ............ 20 Occurrence ..................................... ~ ........................................ __ . 20 Hock :from quarry near Moiliili Chmch ........................................................ 21 Quantitative classification .................................................................. 22 Nephelite basalt and allied rocks ....................· ............................................. 23 Bu.saltic tuffs and ashes of recent eruptions ....... , ............................................... .23 Island of Molokai .................................................................................... 24 Hocks described by Mohle ........................................................................ 24 l~ocks described by Lindgren ..............· ....................... : .............................. 24 Island of Maui ............................... __ ....... __ .... _.............................. _..... __ .. 25 West 1\~faui ................................. _____________ .... ________ .... _. _....... _.... ___ . _.. __ .. _ 25 Bowlders of Waihee Valley ................................................................. 25 Bowlders of lao Valley . ." ................................................................... 26 Rocks described by Mohle .................................................................. 26 Soda trachyte near Lahaina .................................................................. 26 Occurrence and character ............................................................... 26 Che1nical composition ................................................................... 27 Quantitative classification ....... : ...................................................... 28 3 4 CONTENTS. Petrography-Continued. Island of Maui-Continued. Page. East Maui ...................................................................................... 28 Picritic basalt ............................................................................. 28 Occurrence ............................................................................ 28 Description ............................................................................ 28 Chemical composition .................................................................... 29 Qualitative classification ... : ........................................................... 29 Quantitative classification ................................................................. 29 Esse xitic andesite or trachyandesite .................. ·....................................... 30 General character and occurrence ........................................................... 30 Rocks analyzed ........................................................................ 30 Chemical composition ................ : .................................................. 31 Quantitative classification .............................................................. 32 Island of Hawaii ................................................................................... 32 Centers of eruption ............................................................................. 32 Kohala Mountains ............................................................................... 32 Mount Hualalai ................................................................................ 34 Basaltic lavas ............................................................................... 34 Dunite, gabbro, and other granular inclusions in basalt ......................................... 34 Basaltic xenoliths .................... ·........................................................ 35 Trachyte of Puu Waawaa and Anahulu ............................ ; ........................... 35 Mauna Kea ........................... · ............................................................ 36 Rocks described l;>y Cohen ................................................................... 36 Lavas collected by Preston ........................... ·............. · ..................... : ..... 36 Observations of Dutton ..................................................................... 37 Rocks noted by Hitchcock .................... ·.............................................. 37 Rocks described by Daly ................................... : ................. ·............... 37 Other rocks on Mauna Kea ................................................................... 38 Mauna Lo~ ..................................................................................... 38 Rocks described by Cohen .................................· ~ ................................ 38 Rocks described by E. S. Dana ............................................................. 38 Rocks described by Daly .......................................· ............ ~ ................ .. 39 Rocks collected in 1902 ..................................................................... 39 Review .................................................................................... 39 Kilauea ......................................................... ·............................... 39. General statement ............................................ : ................................ 39 Recent lavas ................................................................................ 40 Rocks of the caldera walls ................................................................... 41 Fragments in the tuffs ....................................................................... 42 Gabbro of Uwekahuna "laccolith" ................................................ ·......... .. 43 Summary ......................... :. 43 Puna ..................................... .'..................................................... 43 General discussion........................................................................................ 44 Introduction................ 44 Cha::-acteristics of the rocks............................................................................ 45 Mineral composition
Recommended publications
  • Geochemistry of Sideromelane and Felsic Glass Shards in Pleistocene Ash Layers at Sites 953, 954, and 9561
    Weaver, P.P.E., Schmincke, H.-U., Firth, J.V., and Duffield, W. (Eds.), 1998 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 157 25. GEOCHEMISTRY OF SIDEROMELANE AND FELSIC GLASS SHARDS IN PLEISTOCENE ASH LAYERS AT SITES 953, 954, AND 9561 Andrey A. Gurenko2 and Hans-Ulrich Schmincke2 ABSTRACT Sideromelane and felsic glass shards from unconsolidated Pleistocene volcaniclastic sediments drilled at Sites 953, 954, and 956 are thought to have derived from submarine and subaerial volcanic eruptions on Gran Canaria (Sites 953 and 954) and Tenerife (Sites 954 and 956). We analyzed these glasses by electron microprobe for major elements and sulfur, chlorine, and fluorine. Sideromelane glasses represent a spectrum from alkali basalt through basanite, hawaiite, mugearite, and tephrite to nephelinite. Felsic glasses have compositions similar to benmoreite, trachyte, and phonolite. Vesiculated mafic and felsic glass shards, which are characterized by low S and Cl concentrations (0.01−0.06 wt% S and 0.01–0.04 wt% Cl), are interpreted to have formed by pyroclastic activity on land or in shallow water and appeared to have been strongly degassed. Vesicle-free blocky glass shards having 0.05−0.13 wt% S are likely to have resulted from submarine eruptions at moderate water depths and represent undegassed or slightly degassed magmas. Cl concentrations range from 0.01 to 0.33 wt% and increase with increasing MgO, suggesting that Cl behaves as an incompatible element during magma crystallization. Concentrations of fluorine (0.04− 0.34 wt% F) are likely to represent undegassed values, and the variations in F/K ratios between 0.02 and 0.24 are believed to reflect those of parental magmas and of the mantle source.
    [Show full text]
  • Petrographic Study of a Quartz Diorite Stock Near Superior, Pinal County, Arizona
    Petrographic study of a quartz diorite stock near Superior, Pinal County, Arizona Item Type text; Thesis-Reproduction (electronic); maps Authors Puckett, James Carl, 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 23/09/2021 23:40:37 Link to Item http://hdl.handle.net/10150/554062 PETROGRAPHIC STUDY OF A QUARTZ DIORITE STOCK NEAR SUPERIOR, PINAL COUNTY, ARIZONA by James Carl Puckett, Jr. A Thesis Submitted to the Faculty of the DEPARTMENT OF GEOLOGY In Partial Fulfillment of the Requirements For the Degree of MASTER OF SCIENCE In the Graduate College THE UNIVERSITY OF ARIZONA 1 9 7 0 STATEMENT BY AUTHOR This thesis has been submitted in partial fulfillment of re­ quirements 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 thesis are allowable without special permission, provided that accurate acknowledgment of source is made. Requests for permission for extended quotation from or reproduction 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 judg­ ment the proposed use of the material is in the interests of scholar­ ship. In all other instances, however, permission must be obtained from the author.
    [Show full text]
  • Sugarcane and Lepers: Health Policy and the Colonization of Hawaii (1860-1900)
    Penn History Review Volume 17 Issue 2 Spring 2010 Article 5 May 2010 Sugarcane and Lepers: Health Policy and the Colonization of Hawaii (1860-1900) Emily Kern University of Pennsylvania, [email protected] Follow this and additional works at: https://repository.upenn.edu/phr Recommended Citation Kern, Emily (2010) "Sugarcane and Lepers: Health Policy and the Colonization of Hawaii (1860-1900)," Penn History Review: Vol. 17 : Iss. 2 , Article 5. Available at: https://repository.upenn.edu/phr/vol17/iss2/5 This paper is posted at ScholarlyCommons. https://repository.upenn.edu/phr/vol17/iss2/5 For more information, please contact [email protected]. 78 SUGARCANE AND LEPERS US H EALTH POLICY AND THE COLONIZATION OF HAWAII (1860-1900) Emily Kern INTRODUCTION American involvement in the Hawaiian Islands evolved gradu - ally over the course of the 19 th century in response to the changing political and economic climates of both the islands themselves and of the nascent and expanding continental United States. For many, the US imperial domination in the Pacific was justified as a human - itarian mission, a benevolent ‘civilizing’ effort that combined the vocabulary of democratization with the values of American market capitalism. Although the islands of Hawaii were fundamentally dis - tinct from other major areas of American colonization in the Pacific, most notably the Philippines, the basic ideological and practical mo - tivations which fueled later stages of imperial acquisition evolved to a certain extent over the decades preceding the Spanish-American War as a direct result of American involvement in Hawaii. American advisors in various capacities were a central fixture of the various Hawaiian governments throughout the latter half of the nineteenth century and were thus able to wield enormous influence over the economic and political development of the islands.
    [Show full text]
  • Nonexplosive and Explosive Magma/Wet-Sediment Interaction
    Journal of Volcanology and Geothermal Research 181 (2009) 155–172 Contents lists available at ScienceDirect Journal of Volcanology and Geothermal Research journal homepage: www.elsevier.com/locate/jvolgeores Nonexplosive and explosive magma/wet-sediment interaction during emplacement of Eocene intrusions into Cretaceous to Eocene strata, Trans-Pecos igneous province, West Texas Kenneth S. Befus a,⁎, Richard E. Hanson a, Daniel P. Miggins b, John A. Breyer a, Arthur B. Busbey a a Department of Geology, Texas Christian University, Box 298830, Fort Worth, TX 76129, USA b U.S. Geological Survey, Denver Federal Center, Box 25046, Denver, CO 80225, USA article info abstract Article history: Eocene intrusion of alkaline basaltic to trachyandesitic magmas into unlithified, Upper Cretaceous Received 16 June 2008 (Maastrichtian) to Eocene fluvial strata in part of the Trans-Pecos igneous province in West Texas produced Accepted 22 December 2008 an array of features recording both nonexplosive and explosive magma/wet-sediment interaction. Intrusive Available online 13 January 2009 complexes with 40Ar/39Ar dates of ~47–46 Ma consist of coherent basalt, peperite, and disrupted sediment. Two of the complexes cutting Cretaceous strata contain masses of conglomerate derived from Eocene fluvial Keywords: deposits that, at the onset of intrusive activity, would have been N400–500 m above the present level of phreatomagmatism peperite exposure. These intrusive complexes are inferred to be remnants of diatremes that fed maar volcanoes during diatreme an early stage of magmatism in this part of the Trans-Pecos province. Disrupted Cretaceous strata along Trans-Pecos Texas diatreme margins record collapse of conduit walls during and after subsurface phreatomagmatic explosions.
    [Show full text]
  • Geology and Tectonic Setting of the Kamloops Group, South
    GEOLOGY AND TECTONIC SETTING OF THE KAMLOOPS GROUP, SOUTH- CENTRAL BRITISH COLUMBIA by THOMAS EDWARD EWING B.A., The Colorado College, 1975 M.S., New Mexico Institute of Mining and Technology, 1977 A THESIS SUBMITTED IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY in THE FACULTY OF GRADUATE STUDIES Department of Geological Sciences We accept this thesis as conforming to the required standard THE UNIVERSITY OF BRITISH COLUMBIA February 1981 © Thomas Edward Ewing, 1981 In presenting this thesis in partial fulfilment of the requirements for an advanced degree at the University of British Columbia, I agree that the Library shall make it freely available for reference and study. I further agree that permission for extensive copying of this thesis for scholarly purposes may be granted by the head of my department or by his or her representatives. It is understood that copying or publication of this thesis for financial gain shall not be allowed without my written permission. Department of r.pnlnpiVal Sri PTirp.S The University of British Columbia 2075 Wesbrook Place Vancouver, Canada V6T 1W5 Date February 17, 1981 ABSTRACT The Kamloops Group is a widespread assemblage of Eocene volcanic and sedimentary rocks in south-central British Columbia. Detailed mapping of the type area near Kamloops has resulted in its subdivision into two formations and thirteen formal and informal members. The Tranquille Formation, 0-450 metres thick, consists of lacustrine sediments which grade upward into pillowed flows, hyaloclastite breccia and aquagene tuff. The overlying Dewdrop Flats Formation, with nine members, consists of up to 1000 metres of basalt to andesite phreatic breccia, flow breccia and flat-lying flows.
    [Show full text]
  • Alkalic-Type Epithermal Gold Deposit Model
    Alkalic-Type Epithermal Gold Deposit Model Chapter R of Mineral Deposit Models for Resource Assessment Scientific Investigations Report 2010–5070–R U.S. Department of the Interior U.S. Geological Survey Cover. Photographs of alkalic-type epithermal gold deposits and ores. Upper left: Cripple Creek, Colorado—One of the largest alkalic-type epithermal gold deposits in the world showing the Cresson open pit looking southwest. Note the green funnel-shaped area along the pit wall is lamprophyre of the Cresson Pipe, a common alkaline rock type in these deposits. The Cresson Pipe was mined by historic underground methods and produced some of the richest ores in the district. The holes that are visible along several benches in the pit (bottom portion of photograph) are historic underground mine levels. (Photograph by Karen Kelley, USGS, April, 2002). Upper right: High-grade gold ore from the Porgera deposit in Papua New Guinea showing native gold intergrown with gold-silver telluride minerals (silvery) and pyrite. (Photograph by Jeremy Richards, University of Alberta, Canada, 2013, used with permission). Lower left: Mayflower Mine, Montana—High-grade hessite, petzite, benleonardite, and coloradoite in limestone. (Photograph by Paul Spry, Iowa State University, 1995, used with permission). Lower right: View of north rim of Navilawa Caldera, which hosts the Banana Creek prospect, Fiji, from the portal of the Tuvatu prospect. (Photograph by Paul Spry, Iowa State University, 2007, used with permission). Alkalic-Type Epithermal Gold Deposit Model By Karen D. Kelley, Paul G. Spry, Virginia T. McLemore, David L. Fey, and Eric D. Anderson Chapter R of Mineral Deposit Models for Resource Assessment Scientific Investigations Report 2010–5070–R U.S.
    [Show full text]
  • GEOLOGY of the SLEETMUTE A-5, A-6, B-5, and B-6 QUADRANGLES, SOUTHWESTERN ALASKA by John Decker, R.R
    GEOLOGY OF THE SLEETMUTE A-5, A-6, B-5, AND B-6 QUADRANGLES, SOUTHWESTERN ALASKA by John Decker, R.R. Reifenstuhl, M.S. Robinson, C.F. Waythomas, and J.G. Clough Professional Report 99 1995 Published by Alaska Department of State of Alaska Department of Natural Resources NATURAL DIVISION OF GEOLOGICAL & GEOPHYSICAL SURVEYS GEOLOGY OF THE SLEETMUTE A-5, Ad, B-5, AND B-6 QUADRANGLES, SOUTHWESTERN ALASKA by John Decker, R.R. Reifenstuhl, M.S. Robinson, C.F. Waythomas, and J.G. Clough Professional Report 99 Division of Geological & Geophysical Surveys Cover photo: Northwest-vergent isocline of veryfine-grained sandstone of the Lower(?) and Upper Cretaceous Kuskokwim Group. The outcrop of medium- bedded sandstone is 1.5 miles west of Kiokluk Lake in the Sleetmute B-6 Quadrangle (map unit Kkm). The hammer handle in the photo is 46 cm Fairbanks, Alaska long. Photo by R.R. Reifenstuhl. 1995 STATE OF ALASKA Tony Knowles, Governor DEPARTMENT OF NATURAL RESOURCES John Shively, Commissioner DIVISION OF GEOLOGICAL & GEOPHYSICAL SURVEYS Milton A. Wiltse, Acting Director and State Geologist Division of Geological & Geophysical Surveys publications may be in- spected at the following locations. Address mail orders to the Fairbanks office. Alaska Division of Geological University of Alaska Anchorage Library & Geophysical Surveys 321 1 Providence Drive 794 University Avenue, Suite 200 Anchorage, Alaska 99508 Fairbanks, Alaska 99709-3645 Elmer E. Rasmuson Library Alaska Resource Library University of Alaska Fairbanks 222 W. 7th Avenue Fairbanks, Alaska 99775-1005 Anchorage, Alaska 995 13-7589 Alaska State Library State Office Building, 8th Floor 333 Willoughby Avenue Juneau, Alaska 998 11-057 1 This publication released by the Division of Geological & Geophysical Surveys, text was produced and printed in Fairbanks, Alaska by Graphics North and maps were printed in Colorado Springs, Colorado by Pikes Peak Lithographing Co., at a cost of $9.50 per copy.
    [Show full text]
  • Deadhorse Creek Rare Earth Property
    Deadhorse Creek Rare Earth Property Walsh and Grain Townships Thunder Bay Mining Division, Ontario 48° 51' 7.671" N, 86 39' 45.028" W NTS Mapsheet 42D and 42E Assessment Report Prepared for Canadian International Minerals Inc. Suite 950 – 789 West Pender Street Vancouver, B.C., V6C 1H2 Report Prepared by: 31 October, 2011 1 Contents 1 Contents 1 Contents .......................................................................................................................................................................... 1 2 Figures ............................................................................................................................................................................. 2 3 Tables .............................................................................................................................................................................. 4 4 Summary ......................................................................................................................................................................... 5 5 Introduction .................................................................................................................................................................... 6 6 Reliance on other experts ............................................................................................................................................... 6 7 Property description and location .................................................................................................................................
    [Show full text]
  • THE PETROCHEMISTRY of JAKE M: a MARTIAN MUGEARITE. Stolper
    44th Lunar and Planetary Science Conference (2013) 1685.pdf THE PETROCHEMISTRY OF JAKE_M: A MARTIAN MUGEARITE. Stolper, E.M.1, Baker, M.B.1, Fisk, M.2, Gellert, R.3, King, P.L.4, McLennan, S.M.5, Minitti, M.6, Newcombe, M.1, Schmidt, M.E. 7, Treiman, A.H.8, and the MSL Science Team. 1Caltech, Pasadena, CA 91125, 2Oregon State Univ., 3Univ. Guelph, 4Res. School Earth Sci., ANU, 5SUNY, Stony Brook, 6Applied Phys. Lab., Johns Hopkins Univ., 7Brock Univ., 8Lunar & Planet. Inst. Introduction: Rock “Jake_M” (JM; named for JPL The surface of JM was not brushed or abraded prior engineer Jake Matijevic) was the first sample analyzed to analysis, so the APXS analyses probably include by the Alpha Particle X-ray Spectrometer (APXS) in- contributions from surface coatings, including adhering strument on MSL [1]. Although it is an isolated frag- dust, and these are the probable source of the S and Cl ment lacking field context, its dark color and apparently in JM. Experience with MER, however, indicates that fine-grained texture suggested it was a relatively homo- the characteristics of rock compositions are typically geneous igneous rock and thus an appropriate sample to not obscured by surface components, and the levels of S initiate the APXS analytical program. We report here and Cl in JM are lower than virtually all unbrushed the preliminary APXS analyses of JM and a plausible analyses from the Spirit rover and lower than many of interpretation of their significance for petrogenesis. the brushed analyses, so the level of surface contamina- Results: Three spots on JM were analyzed with the tion and alteration are likely relatively minor [5].
    [Show full text]
  • Plate Tectonics, Volcanic Petrology, and Ore Formation in the Santa Rosalia Area, Baja California, Mexico
    Plate tectonics, volcanic petrology, and ore formation in the Santa Rosalia area, Baja California, Mexico Item Type text; Thesis-Reproduction (electronic) Authors Schmidt, Eugene Karl, 1947- 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 01/10/2021 01:50:58 Link to Item http://hdl.handle.net/10150/555057 PLATE TECTONICS, VOLCANIC PETROLOGY, AND ORE FORMATION IN THE SANTA ROSALIA AREA, BAJA CALIFORNIA, MEXICO by Eugene Karl Schmidt A Thesis Submitted to the Faculty of the DEPARTMENT OF GEOSCIENCES In Partial Fulfillment of the Requirements For the Degree of MASTER OF SCIENCE In the Graduate College THE UNIVERSITY OF ARIZONA 1 9 7 5 z- STATEMENT BY AUTHOR This thesis has been submitted in partial ful­ fillment 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 thesis are allowable without special permission, provided that accurate ac­ knowledgment of source is made. Requests for permission for extended quotation from or reproduction of this manu­ script 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 judgment the proposed use of the material is in the interests of scholarship. In all other instances, however, permission must be obtained from the author.
    [Show full text]
  • Igneous Rocks —!Some Minerals Form During Weathering Processes
    Minerals Give Clues To Their Environment Of Formation !!Can be a unique set of conditions to form a particular mineral or rock !!Temperature and pressure determine conditions to form diamond or graphite (polymorphs) !! Diamonds require pressures and temperatures equivalent to those in the mantle at least 150 km below Earth’s surface. !! Diamond is metastable Figure 3.31 Also Rocks: Mixtures of Minerals !!Clues to climate: !!Igneous rocks —!Some minerals form during weathering processes. !!Formed by solidification of magma. —!Past climates can be determined from the kinds of !!Sedimentary rocks minerals preserved in sedimentary rocks. !! !!Clues to seawater composition: Formed by sedimentation of materials transported in solution or suspension. —!The content of past seawater can be determined from minerals formed when the seawater evaporated and !!Metamorphic rocks deposited its salts. !!Formed by the alteration of preexisting sedimentary or igneous rocks in response to increased pressure and temperature. Distinguishing The Three Rock Types Texture and Mineral Assemblage The differences among rock types are identified !!A systematic description of a rock includes both by two features. texture and mineral assemblage. !!Texture: !!Megascopic textural features of rocks are those —!The overall appearance of a rock due to the size, shape, that we can see with the unaided eye. and arrangement of its constituent mineral grain. !!Microscopic textural features of rocks are those !!Mineral assemblage: that require high magnification to be viewed. —!The type and abundance of the minerals making up a rock. Figure 3.32 Figure 3.32 A B Figure 3.32 Figure 3.32 D C Mineral Concentration !!Two common processes of concentration: !!Fluids released by a cooling body of magma.
    [Show full text]
  • TERTIARY MAGMATISM in NORTHERN SARDINIA by Michael
    TERTIARY MAGMATISM IN NORTHERN SARDINIA by Michael John Rutter A Thesis submitted for the Degree of Doctor of Philosophy, University of London Department of Geology, Imperial College of Science & Technology, Prince Consort Road, LONDON SW7. ABSTRACT Tertiary magmatism in northern Sardinia is dominated by a temporal transition from subduction-related (29.9-13 Ma) to extensional (5-0.12 Ma) volcanism. Geochemical parameters of lavas, independent of any differentiation processes, have been used to constrain the changing chemical characteristics of magma-producing source mantle beneath Sardinia, during and after active subduction. Late Oligocene and Miocene (29.9-13 Ma) basalt-andesite- dacite-rhyolite lavas were associated with active subduction, to the east of the Sardinia continental block. They are associated with contemporaneous extension, possibly in a back-arc environment, which facilitated passage of magmas to the surface, and high-T low-P fractionation of an anhydrous gabbroic mineral assemblage. Low K/Cs and high Ba/La ratios in Sardinian subduction-related magmas, may reflect the influx of fluids or melts, derived from the subducted slab, into their mantle source. Low Nb and Ta abundances can be explained by the retention of these elements in some residual phase, stable under the hydrous conditions which may exist in the mantle wedge, although this phase is probably not titaniferous. High LILE-HFSE ratios may represent the addition of LILE-enriched fluids or melts from the subducted oceanic lithosphere to MORB-source mantle, or to magma generation in OIB-source mantle. Following a gap in magmatic activitiy, volcanism resumed in the Pliocene with the eruption of high-Al basalt, dacite and rhyolite lavas, which require the persistence of subduction-related source mantle beneath Sardinia at least 8 Ma after the cessation of active subduction.
    [Show full text]