Mantle Metasomatism and the Generation of Alkaline
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Mineralogy and Chemistry of Rare Earth Elements in Alkaline Ultramafic Rocks and Fluorite in the Western Kentucky Fluorspar District Warren H
University of Kentucky UKnowledge Kentucky Geological Survey Report of Kentucky Geological Survey Investigations 6-2019 Mineralogy and Chemistry of Rare Earth Elements in Alkaline Ultramafic Rocks and Fluorite in the Western Kentucky Fluorspar District Warren H. Anderson University of Kentucky, [email protected] Right click to open a feedback form in a new tab to let us know how this document benefits oy u. Follow this and additional works at: https://uknowledge.uky.edu/kgs_ri Part of the Geology Commons Repository Citation Anderson, Warren H., "Mineralogy and Chemistry of Rare Earth Elements in Alkaline Ultramafic Rocks and Fluorite in the Western Kentucky Fluorspar District" (2019). Kentucky Geological Survey Report of Investigations. 55. https://uknowledge.uky.edu/kgs_ri/55 This Report is brought to you for free and open access by the Kentucky Geological Survey at UKnowledge. It has been accepted for inclusion in Kentucky Geological Survey Report of Investigations by an authorized administrator of UKnowledge. For more information, please contact [email protected]. Mineralogy and Chemistry of Rare Earth Elements in Alkaline Ultramafic Rocks and Fluorite in the Western Kentucky Fluorspar District Warren H. Anderson Report of Investigations 8 doi.org/10.13023/kgs.ri08.13 Series XIII, 2019 Cover Photo: Various alkaline ultramafic rocks showing porphyritic, brecciated, and aphanitic textures, in contact with host limestone and altered dike texture. From left to right: • Davidson North dike, Davidson core, YH-04, 800 ft depth. Lamprophyre with calcite veins, containing abundant rutile. • Coefield area, Billiton Minner core BMN 3. Intrusive breccia with lamprophyric (al- nöite) matrix. • Maple Lake area, core ML-1, 416 ft depth. -
Mineralogy and Geochemistry of Ocelli in the Damtjernite Dykes and Sills, Chadobets Uplift, Siberian Craton: Evidence of the Fluid–Lamprophyric Magma Interaction
minerals Article Mineralogy and Geochemistry of Ocelli in the Damtjernite Dykes and Sills, Chadobets Uplift, Siberian Craton: Evidence of the Fluid–Lamprophyric Magma Interaction Anna A. Nosova 1,*, Ludmila V. Sazonova 1,2, Alexey V. Kargin 1 , Elena O. Dubinina 1 and Elena A. Minervina 1 1 Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry, Russian Academy of Sciences (IGEM RAS), 119017 Moscow, Russia; [email protected] (L.V.S.); [email protected] (A.V.K.); [email protected] (E.O.D.); [email protected] (E.A.M.) 2 Geology Department, Lomonosov Moscow State University, 119991 Moscow, Russia * Correspondence: [email protected]; Tel.:+7-499-230-8414 Abstract: The study reports petrography, mineralogy and carbonate geochemistry and stable iso- topy of various types of ocelli (silicate-carbonate globules) observed in the lamprophyres from the Chadobets Uplift, southwestern Siberian craton. The Chadobets lamprophyres are related to the REE-bearing Chuktukon carbonatites. On the basis of their morphology, mineralogy and relation with the surrounding groundmass, we distinguish three types of ocelli: carbonate-silicate, containing carbonate, scapolite, sodalite, potassium feldspar, albite, apatite and minor quartz ocelli (K-Na-CSO); carbonate–silicate ocelli, containing natrolite and sodalite (Na-CSO); and silicate-carbonate, con- taining potassium feldspar and phlogopite (K-SCO). The K-Na-CSO present in the most evolved Citation: Nosova, A.A.; Sazonova, damtjernite with irregular and polygonal patches was distributed within the groundmass; the patches L.V.; Kargin, A.V.; Dubinina, E.O.; consist of minerals identical to minerals in ocelli. Carbonate in the K-Na-CSO are calcite, Fe-dolomite Minervina, E.A. -
Geology of Diamond Occurrences at Southern Knee Lake, Oxford Lake
80 a Diamond inclusion KL-2 and intergrowth field Summary and guide to figures 70 KL-3 In 2016, bedrock mapping and sampling by the Manitoba Geological Survey resulted Indicator minerals in the conglomerate (MGS sample LX/KL-2) consist of chromite 60 Argyle lo Geology of diamond occurrences at southern Knee Lake, Oxford Lake–Knee Lake lamproite in the discovery of microdiamonds in shoreline outcrop at southern Knee Lake – a and Cr-spinel, whereas the lapilli tuff (MGS sample LX/KL-3) contains chromite, Cr- eo gic g a 50 a l discovery since confirmed and extended by Altius Minerals Corp. (press release, diopside, Cr-spinel and diamond-inclusion Cr-spinel, indicative of a mantle-derived b s 2 3 u o Cr O (wt. %) September 25, 2017). The microdiamonds are hosted by polymictic volcanic magmatic precursor sourced from within the diamond stability field (>140 km 40 t r i v conglomerate and volcanic sandstone belonging to the Oxford Lake group (ca. 2.72 depth). Indicator mineral compositions (Figures 18 & 19), coupled with the absence n e a MGS HP y greenstone belt, Manitoba (NTS 53L14, 15) Kimberlite Ga) of the Oxford Lake–Knee Lake greenstone belt in the northwestern Superior of garnet and ilmenite, suggest that the magmatic precursor was not kimberlitic. 30 province (Figures 1–5). Well-preserved primary features (Figures 6–8) indicate m 20 deposition as debris and turbidity flows in an alluvial or shallow-marine fan setting, Microdiamonds (n = 144; Figures 20 & 21) obtained from a 15.8 kg sample of the 1928 S.D. -
The Genesis of Ultramafic Lamprophyres
THE GENESIS OF ULTRAMAFIC LAMPROPHYRES Stephen F. Foley1 and Alexandre V. Andronikov2 1 University of Greifswald, Germany; 2 University of Michigan, U.S.A. ultramafic lamprophyre, and attempts to find conditions ULTRAMAFIC LAMPROPHYRE TYPES of pressure, temperature, fO2 and volatile mixtures that permit stabilization of all the peridotite minerals AND THEIR CLASSIFICATION together at the liquidus. If successful, results from these two approaches will agree about all conditions of origin The ultramafic lamprophyres form a heterogeneous of the melt. group of alkaline rocks whose origin has never been adequately explained. They are generally attributed to However, this interpolation has been shown to be melting of carbonate-bearing peridotites, but details are problematic for alkaline and volatile-rich rocks because lacking as to how and why the parental melts for of the large number of varaibles and the near- various ultramafic lamprophyres differ. The commonest impossibility of identifying the liquid compositions ultramafic lamprophyres are alnöites (melilite- exactly in near-solidus experiments on peridotite. A dominated) and aillikites (carbonate-dominated). In his large number of experiments on peridotite with mixed review of lamprophyres, Rock (1991) concluded these volatiles were conducted in the late 1970s and early two groups are derived from distinct types of primary 1980s (e.g. Wyllie 1978; Eggler 1978; Olafsson and mantle-derived melts. The nomenclature of these rocks Eggler, 1983) but these have only been able to give is confused and has often changed: recent IUGS general pointers as to the type of melts produced, and recommendations have tried to solve this by cannot distinguish in any detail between melts such as dismantling the lamprophyre construct, assigning kimberlites, melilitites, carbonatites and the different alnöites to the melilitites and aillikites to the types of ultramafic lamprophyres. -
A MODEL for BIOMASS ASSESSMENT E-023 SUBMITTED BY: Dr
• A MODEL FOR BIOMASS ASSESSMENT E-023 SUBMITTED BY: Dr. Stephen J. Walsh Associate Professor Dr. George p. Malanson Assistant Professor Dr. John D. Vitek Associate Professor Dr. David R. Butler Assistant Professor Department of Geography Oklahoma State University & in conjunction with USDA/Agricultural Research Service SUBMITTED TO: Dr. Norman N. Durham, Director Water Research Center Oklahoma State University March 14, 1983 Introduction The surface of the earth is a complex system responding to the input of energy, natural and human. Human use of the surface for maximum agricultural efficiency requires knowledge of the interactions of all variables involved in the system. Broad categories of phenomena, including the atmosphere (weather and climate), biosphere (vegetation, fauna, and human activity), hydrosphere (precipitation, runoff, infiltration, fluvial erosion, and evapotranspiration), and the lithosphere (soil, topography, and parent material), can be identified as the major variables in any assessment. Assessment of interactions requires data from various sources. The emergence of remote sensing as a source of data for assessments in the last decade permits the development of more accurate predictive models. Refinements in data acquisition, such as improved resolution, the use of radar, and the correlation of detailed surface observations with satellite overpasses, provide researchers with the capability to assess inter relationships and create accurate models. A conceptual model, Figure 1, illustrates the interaction of the Department of Geography/CARS and the USDA/Agricultural Research Service with components of the natural system for the purpose of creating a predictive model for biomass assessment~~CARS, the remote sensing center at Oklahoma State University, plus ARS of the USDA bring different skills to this joint research effort. -
Summits on the Air – ARM for USA - Colorado (WØC)
Summits on the Air – ARM for USA - Colorado (WØC) Summits on the Air USA - Colorado (WØC) Association Reference Manual Document Reference S46.1 Issue number 3.2 Date of issue 15-June-2021 Participation start date 01-May-2010 Authorised Date: 15-June-2021 obo SOTA Management Team Association Manager Matt Schnizer KØMOS Summits-on-the-Air an original concept by G3WGV and developed with G3CWI Notice “Summits on the Air” SOTA and the SOTA logo are trademarks of the Programme. This document is copyright of the Programme. All other trademarks and copyrights referenced herein are acknowledged. Page 1 of 11 Document S46.1 V3.2 Summits on the Air – ARM for USA - Colorado (WØC) Change Control Date Version Details 01-May-10 1.0 First formal issue of this document 01-Aug-11 2.0 Updated Version including all qualified CO Peaks, North Dakota, and South Dakota Peaks 01-Dec-11 2.1 Corrections to document for consistency between sections. 31-Mar-14 2.2 Convert WØ to WØC for Colorado only Association. Remove South Dakota and North Dakota Regions. Minor grammatical changes. Clarification of SOTA Rule 3.7.3 “Final Access”. Matt Schnizer K0MOS becomes the new W0C Association Manager. 04/30/16 2.3 Updated Disclaimer Updated 2.0 Program Derivation: Changed prominence from 500 ft to 150m (492 ft) Updated 3.0 General information: Added valid FCC license Corrected conversion factor (ft to m) and recalculated all summits 1-Apr-2017 3.0 Acquired new Summit List from ListsofJohn.com: 64 new summits (37 for P500 ft to P150 m change and 27 new) and 3 deletes due to prom corrections. -
Magmatic Evolution and Petrochemistry of Xenoliths Contained Within an Andesitic Dike of Western Spanish Peak, Colorado
Magmatic Evolution and Petrochemistry of Xenoliths contained within an Andesitic Dike of Western Spanish Peak, Colorado Thesis for Departmental Honors at the University of Colorado Ian Albert Rafael Contreras Department of Geological Sciences Thesis Advisor: Charles Stern | Geological Sciences Defense Committee: Charles Stern | Geological Sciences Rebecca Flowers | Geological Sciences Ilia Mishev | Mathematics April the 8th 2014 Magmatic Evolution and Petrochemistry of Xenoliths contained within an Andesitic Dike of Western Spanish Peak, Colorado Ian Albert Rafael Contreras Department of Geological Sciences University of Colorado Boulder Abstract The Spanish Peaks Wilderness of south-central Colorado is a diverse igneous complex which includes a variety of mid-Tertiary intrusions, including many small stocks and dikes, into Cretaceous and early Tertiary sediments. The focus of this thesis is to determine whether gabbroic xenoliths found within an andesitic dike on Western Spanish Peak were accidental or cognate, and their implications for the magma evolution of the area. A total of twelve samples were collected from a single radial dike, eleven of which were sliced into thin sections for petrological analyses. From the cut thin sections, six were chosen for electron microprobe analysis to determine mineral chemistry, and billets of ten samples were subject to ICP-MS analysis to determine bulk rock, trace element chemistry. Xenoliths were dominated by amphiboles, plagioclase feldspars, clinopyroxenes and opaques (Fe-Ti oxides) distributed in mostly porphyritic to equigranular textures. Pargasitic and kaersutitic amphiboles are present in both the xenoliths and the host dike. Additionally, plagioclase feldspars range from albite to labradorite, and clinopyroxenes range from augite to diopside. All xenoliths were found to be enriched in elements Ti, Sr, Cr and Mn compared to the host dike and other Spanish Peak radial dikes. -
Preliminary Evaluation of Potential Acecs---Royal
Preliminary Evaluation of Potential ACECs—Royal Gorge Field Office Relevance and Importance Criteria Prepared by U.S. Department of the Interior Bureau of Land Management Royal Gorge Field Office Cañon City, CO February 2017 This page intentionally left blank Preliminary Evaluation of Potential iii ACECs—Royal Gorge Field Office Table of Contents Acronyms and Abbreviations ....................................................................................................... ix Executive Summary ...................................................................................................................... xi _1. Introduction .............................................................................................................................. 1 _1.1. Eastern Colorado Resource Management Plan ............................................................... 1 _1.2. Authorities ....................................................................................................................... 1 _1.3. Area of Consideration ..................................................................................................... 1 _1.4. The ACEC Designation Process ..................................................................................... 1 _2. Requirements for ACEC Designation .................................................................................... 3 _2.1. Identifying ACECs .......................................................................................................... 5 _2.2. Special Management -
Chronology of Late Cretaceous Igneous and Hydrothermal Events at the Golden Sunlight Gold-Silver Breccia Pipe, Southwestern Montana
Chronology of Late Cretaceous Igneous and Hydrothermal Events at the Golden Sunlight Gold-Silver Breccia Pipe, Southwestern Montana U.S. GEOLOGICAL SURVEY BULLETIN 2155 T OF EN TH TM E R I A N P T E E D R . I O S . R U M 9 A 8 4 R C H 3, 1 a Chronology of Late Cretaceous Igneous and Hydrothermal Events at the Golden Sunlight Gold-Silver Breccia Pipe, Southwestern Montana By Ed DeWitt, Eugene E. Foord, Robert E. Zartman, Robert C. Pearson, and Fess Foster T OF U.S. GEOLOGICAL SURVEY BULLETIN 2155 EN TH TM E R I A N P T E E D R . I O S . R U M 9 A 8 4 R C H 3, 1 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1996 a U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Gordon P. Eaton, Director For sale by U.S. Geological Survey, Information Services Box 25286, Federal Center Denver, CO 80225 Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government Library of Congress Cataloging-in-Publication Data Chronolgy of Late Cretaceous igneous and hydrothermal events at the Golden Sunlight gold-silver breccia pipe, southwestern Montana / by Ed DeWitt . [et al.]. p. cm.—(U.S. Geological Survey bulletin ; 2155) Includes bibliographical references. Supt. of Docs. no. : I 19.3 : 2155 1. Geology, Stratigraphic—Cretaceous. 2. Rocks, Igneous—Montana. 3. Hydrothermal alteration—Montana. 4. Gold ores—Montana. 5. Breccia pipes—Montana. -
Frozen Ground
Frozen Ground Th e News Bulletin of the International Permafrost Association Number 32, December 2008 INTERNATIONAL PERMAFROST ASSOCIATION Th e International Permafrost Association, founded in 1983, has as its objectives to foster the dissemination of knowledge concerning permafrost and to promote cooperation among persons and national or international organisations engaged in scientifi c investigation and engineering work on permafrost. Membership is through national Adhering Bodies and Associate Members. Th e IPA is governed by its offi cers and a Council consisting of representatives from 26 Adhering Bodies having interests in some aspect of theoretical, basic and applied frozen ground research, including permafrost, seasonal frost, artifi cial freezing and periglacial phenomena. Committees, Working Groups, and Task Forces organise and coordinate research activities and special projects. Th e IPA became an Affi liated Organisation of the International Union of Geological Sciences (IUGS) in July 1989. Beginning in 1995 the IPA and the International Geographical Union (IGU) developed an Agreement of Cooperation, thus making IPA an affi liate of the IGU. Th e Association’s primary responsibilities are convening International Permafrost Conferences, undertaking special projects such as preparing databases, maps, bibliographies, and glossaries, and coordinating international fi eld programmes and networks. Conferences were held in West Lafayette, Indiana, U.S.A., 1963; in Yakutsk, Siberia, 1973; in Edmonton, Canada, 1978; in Fairbanks, Alaska, 1983; in Trondheim, Norway, 1988; in Beijing, China, 1993; in Yellowknife, Canada, 1998, in Zurich, Switzerland, 2003, and in Fairbanks, Alaska, in 2008. Th e Tenth conference will be in Tyumen, Russia, in 2012.Field excursions are an integral part of each Conference, and are organised by the host Executive Committee 2008-2012 Council Members Professor Hans-W. -
APPENDIX a APPENDIX a Tiliber SALE Sumllary
APPENDIX A APPENDIX A TIliBER SALE SuMllARY Area r.ocarmn -“anagemenr Area Treatmentl Esrlmated Probable Harvest -RIS I.ocatmn Area Volume “ethods by -Towashw & Range* (Acres) m LlpiBF Forest Type 1984 leadvllle 28 30 57 02 lodgepole pine 100210 clearcut T9S, R80W 1984 Leadvllle 2B 30 86 03 Lodgepole pne 100210 clearcut T8S. mow 1984 Leadvllle 70 50 143 03 bdgepole pule 100203 clearcur; spruce,fr ms, R80W shelterwood 1984 Leadvllle lhstrxt-vlde 80 2.29 08 All species. approprrare for nanagement Area.*=C 1984 Sahda 4B 320 457 16 Spruce,flr group 101001; 101002 selectmn T14S, R80W 1984 Sallda 40 200 114 0.4 Douglas-*rr thmnmg; 102311 lodgepole pine and T48N, WE aspen. clearcur 1984 SalIda 5B 15 29 0 1 Lodgepole pm 102211 clearcur T49N, R7E 1984 Salzda 5B 30 86 0.3 Aspen: clearcut 1027.06 public fuelwood T49N, WE 1984 Sahd.9 40 25 86 0.3 Aspen clearcur 101301 public fuelwood T13S, R77W 1984 Sahda District-wide 320 200 0.7 All species approprrate for nanagement Area 1984 San Carlas ,A 318 loo0 3.5 Spruce,fx. clearcut; 103510 Douglas-fir: two-step T24S, R69W sheltewood 1984 San carkss rhstrzct-wrde 420 257 0.9 All Epecles appropriate for Management Area 1984 Pxkes Peak WE 314 143 0.3 Ponderosa pine and 115302. 113303 Douglas-cr. Two-step TI1S. R68W shelterwad; spruce/ fm and aspen clearcut 1984 PlkS Peak 7A 476 286 10 Douglas-fm and 117101, 117102, ponderosa pme two- 117401, 11,402 step shelterwood, T11 s; 12s. wow aspen. clearcur *All Townshq and Range ~~rar~ons refer to the New “exzco and Sxcth Prmcxpal “enduas, ““Ifed States survey “See Chapter III, Management Area Preserqrmns for harvest methods by specks A-l TIMBER SALE SuMEwlY Area hcatlo” -Managemn Area Treatment Estmated Probable Harverr Hlscal -RI8 locatloo Area Yolme Methods by Year: District Sale Name -Township 6 Ranae (Acres) gcJ MMBF Forest Type 1984 Pikes Peak .Jobos Gulch 1OR 450 286 I.0 Poaderosa pm.e 116701, 116002 two-step shelterwood T118, R69” 1984 Pikes Peak Quaker RLdgs 28 250 143 0.5 Ponderoaa pme TWO- 116601. -
Co-Raton-Mesa-Nm.Pdf
D-5 I I I~ ..--- ~..,.....----~__O~~--- I I I UNITED STATES DEPARTMENT OF THE INTERIOR NATIONAL SE I I I I II I Cover painting "FISHERS PEAK" by Arthur Roy Mitchell, commissioned for the Denver Post's Collection of Western Art, reproduced through the courtesy of Palmer Hoyt, Editor. I I.1 I I SYNOPSIS NOT FOR FU~LIC l{ELEASJ Raton Mesa near Trinidad, Colorado, about 200 miles south of Denver, I is the highest, most scenic, impressive and accessible of a scattered group of lava-capped mesas straddling the eastern half of the Colorado- I New Mexico boundary. It and its highest part, Fishers Peak, are well I known landmarks dating back to the days of the Santa Fe Trail which~ traverses Raton Pass on its southwest flank, today crossed by an interstate high- I way. Three distinct, easily recognized vegetative zones, mostly forest, lay on its slopes; the Mesa top is a high mountain grassland. I Ancient lava flows covered portions of this region, the Raton I section of the Great Plains physiographic province, millions of years ago when the surface was much higher. These flows protected the mesas from subsequent erosion which has carried away the surrounding territory, • leaving Fishers Peak today towering 4,000 feet above the City of Trinidad. I Lavas at Capulin Mountain, a National Monument located nearby in New I Mexico, though at a lower elevation, are thought to be much more recent. Raton Pass was a strategic point on the Mountain Branch of the I Santa Fe Trail during the Mexican and Civil Wars, and to travelers past and present a clima~~ gateway to the southwest.