Mantle-Crust Interaction in Granite

Total Page:16

File Type:pdf, Size:1020Kb

Mantle-Crust Interaction in Granite University of South Florida Scholar Commons Graduate Theses and Dissertations Graduate School 11-19-2014 Mantle-crust Interaction in Granite Petrogenesis in Post-collisional Settings: Insights from the Danubian Variscan Plutons of the Romanian Southern Carpathians Ciprian Cosmin Stremtan University of South Florida, [email protected] Follow this and additional works at: https://scholarcommons.usf.edu/etd Part of the Geochemistry Commons, and the Geology Commons Scholar Commons Citation Stremtan, Ciprian Cosmin, "Mantle-crust Interaction in Granite Petrogenesis in Post-collisional Settings: Insights from the Danubian Variscan Plutons of the Romanian Southern Carpathians" (2014). Graduate Theses and Dissertations. https://scholarcommons.usf.edu/etd/5624 This Dissertation is brought to you for free and open access by the Graduate School at Scholar Commons. It has been accepted for inclusion in Graduate Theses and Dissertations by an authorized administrator of Scholar Commons. For more information, please contact [email protected]. Mantle-crust Interaction in Granite Petrogenesis in Post-collisional Settings: Insights from the Danubian Variscan Plutons of the Romanian Southern Carpathians by Ciprian Cosmin Stremțan A dissertation submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy School of Geosciences College of Arts and Sciences University of South Florida Co-Major Professor: Jeffrey G. Ryan, Ph.D. Co-Major Professor: Paul Wetmore, Ph.D. Jonathan G. Wynn, Ph.D. Ioan Balintoni, Ph.D. Date of Approval: November 19, 2014 Keywords: granitoid, continental crust, delamination, trace elements, isotopes Copyright © 2014, Ciprian Cosmin Stremțan DEDICATION To all the wonderful people who made this possible. TABLE OF CONTENTS List of Tables ................................................................................................................................. iv List of Figures ................................................................................................................................. v Abstract ........................................................................................................................................ viii Chapter One: Post-collisional Late Variscan Magmatism in the Danubian Domain (South Carpathians, Romania) Documented by Zircon U/Pb LA-ICP-MS .............................. 1 Note to Reader .................................................................................................................... 1 Abstract ............................................................................................................................... 1 Introduction ......................................................................................................................... 2 Variscan Orogeny: Plate Tectonics Concepts and Timing ................................................. 3 Geological Setting ............................................................................................................... 6 Alpine Structure of the South Carpathians ............................................................. 6 Pre-Variscan Structure of the South Carpathians ................................................... 7 Variscan Events in South Carpathians .................................................................... 8 Samples and Analytical Methods........................................................................................ 9 Samples ................................................................................................................... 9 Analytical Methods ............................................................................................... 11 Results ............................................................................................................................... 13 Discussion ......................................................................................................................... 17 General Plate Tectonics Concept .......................................................................... 17 Major Element Geochemistry ............................................................................... 18 Trace Elements and Isotopic Data ........................................................................ 20 Delamination Model ............................................................................................. 21 Conclusions ....................................................................................................................... 24 References ......................................................................................................................... 25 Chapter Two: Petrology and Geochemistry of the Late Variscan Post-collisional Furcătura Granitic Pluton South. Carpathian Mts. (Romania). ............................................................... 34 Abstract ............................................................................................................................. 34 Introduction ....................................................................................................................... 35 i Geological Setting ............................................................................................................. 37 Samples and Petrography .................................................................................................. 40 Analytical Methods ........................................................................................................... 43 Major and Trace Elements .................................................................................... 43 Oxygen Isotopes.................................................................................................... 44 Strontium and Neodymium Isotopes .................................................................... 45 Results ............................................................................................................................... 46 Whole-rock Geochemistry .................................................................................... 46 Isotope Geochemistry ........................................................................................... 54 Discussion ......................................................................................................................... 55 P-Tº Conditions of Granitoid Formation .............................................................. 55 Petrogenesis .......................................................................................................... 57 Timing of the Pluton Emplacement and Comparison with the Variscan Events from Central-Western Europe ......................................................................... 68 Geodynamic Implications ..................................................................................... 69 Conclusions ....................................................................................................................... 73 References ......................................................................................................................... 74 Chapter Three: Post Collisional Magmatism Associated with Variscan Orogeny in the Danubian Domain (Romanian Southern Carpathians): the Motru Dyke Swarm ................... 92 Abstract ............................................................................................................................. 92 Introduction ....................................................................................................................... 93 Geological setting ............................................................................................................. 95 Analytical Methods ........................................................................................................... 97 Major and Trace Elements .................................................................................... 97 Radiogenic Isotopes .............................................................................................. 98 Results ............................................................................................................................... 99 Samples and Petrology .......................................................................................... 99 Bulk-rock Geochemistry ..................................................................................... 100 Bulk-rock Sr-Nd Isotope Geochemistry ............................................................. 108 Discussion ....................................................................................................................... 109 Timing of the MDS Intrusion ............................................................................. 109 Petrogenesis ........................................................................................................ 112 Mode of MDS Formation.................................................................................... 119 Conclusions ..................................................................................................................... 120 ii References ....................................................................................................................... 121 Chapter Four: The Role of the Continental Crust and Lithospheric Mantle in Variscan Post- Collisioanl Magmatism – Insights from Muntele Mic, Ogradena, Cherbelezu, Sfârdinu, and Culmea Cernei Plutons (Romanian
Recommended publications
  • Sülfür Throughout Geological Time in Balkan Peninsula**
    Mineral Res. Expl. Bul.. 123-124. 1-12, 2002 SÜLFÜR THROUGHOUT GEOLOGİCAL TIME IN BALKAN PENINSULA** Radule POPOVİC* ABSTRACT.- During investigations for a long time it has been remarked that the oldest metallogenic epochs in Balkan Peninsula include a limited number of, occurrences with sülfür as one of the chief chemical elements. Thus it could be said that in these epochs the deposits with sulphur compounds either have not been formed or in some cases there were only rare showings. So, for instance with the Grenvilian epoch, according to date know- ledge, only one occurrence in Pelagonids (Nezilovo) could be associated. In the Baikalian metallogenic epoch, characterized by formation of greenschists in western Macedonian only traces of sulfide mineralizations, then one deposit of lead, zinc and copper sulfides, as well as one pyrite impregnation in the larger Popcevo - Dojran area (eastern Macedonia), exhibiting sülfür content less than 0,11% are present. In contrast to Pelagonian-Rhodopean massif, in the Green complex (Vlasina) of eastern Serbia numerous deposits and occurrences of pyrite and lead, zinc and copper sulfides are present, indicating a more remarkable sülfür yield in this district during Baikalian metallogenic epoch. Thanks to this fact it could be estimated this epoch to be much more enriched in sülfür in Balkan Peninsula, compared with the Grenvilian epoch. In the next epochs (Caledonian and Hercynian) the sülfür yield had become more and more intensive. This is especially related to the phytlitic volcanogenic-sedimentary origin formation of western Macedonian. in which fifteen deposits and occurrences of lead. zinc, copper and molybdenum sulfides have been registered, indicating numerous richer and poorer, certainly irregular pyrite impregnations.
    [Show full text]
  • Vrancea and Hindu Kush Areas of Mantle Earthquakes: Comparative Tectonic Analysis
    Scientific Annals, School of Geology, Aristotle University of Thessaloniki Thessaloniki Special volume 99 51-56 Proceedings of the XIX CBGA Congress, Thessaloniki, Greece 2010 VRANCEA AND HINDU KUSH AREAS OF MANTLE EARTHQUAKES: COMPARATIVE TECTONIC ANALYSIS Trifonov V.G.1, Ivanova T.P.2, Bachmanov D.M.3 1Geological Institute of the RAS, 7 Pyzhevsky, Moscow 119017 Russia; [email protected]; [email protected] 2Institute of Dynamics of Geospheres of the RAS, B. 6, 38 Leninsky Ave., Moscow 117334 Russia; [email protected] 3Geological Institute of the RAS, 7 Pyzhevsky, Moscow 119017 Russia; [email protected] Abstract: The Late Cenozoic tectonics in the Eastern Carpathians and the Pamir-Hindu Kush region are compared to ascertain structural position and origin of strong mantle earthquakes in the Vrancea and Hundu Kush megasources. Intensive Oligocene–Quaternary deformation took place in the Pamir-Hindu Kush region. Under compressive regime, large upper crust blocks were detached and displaced up to several hundred kilometers. Relics of the oceanic crust of the Precambrian, Hercynian Paleo-Tethys and Early Meso-Tethys were overthrusted by the upper crust blocks and subsided to the depth of 40–70 km, where they were metamorphosed into higher density metabasites of the granulite-eclogite type. In the Pliocene–Quaternary, the region was quickly elevated, mainly because of decrease of density of the up- per mantle. As a result, the detached dense metabasite slab began to move down to the depths of 270– 300 km. The same processes took place in the Vrancea area. The basic rocks of the Inner Carpathian zones were moved and underthrusted the Moesian Platform with simultaneous overthrusting by the Out- er Carpathian zone.
    [Show full text]
  • Tüm Dergi Için Tıklayınız
    Yerbilimleri, 31 (1), 1–22 Hacettepe Üniversitesi Yerbilimleri Uygulama ve Araştırma Merkezi Dergisi Journal of the Earth Sciences Application and Research Centre of Hacettepe University General correlation of the Late Palaeozoic sequences in the Balkans and the Caucasus Balkanlarda ve Kafkaslardaki Üst Paleozoyik istiflerinin genel karşılaştırması Slavcho YANEV1, Shota ADAMIA2 1Geological Institute of the Bulgarian Academy of Sciences, “Acad. G. Bonchev” Str. Bl. 24, 1113 Sofia, BULGARIA 2State University of Tbilisi, Department of Geology and Palaeontology, Chavchavadze av. 1, 380028, Tbilisi, GEORGIA. Geliş (received) : 09 Haziran (June) 2009 Kabul (accepted) : 07 Kasım (November) 2009 ABSTRACT This paper presents a brief correlation of the Late Palaeozoic (mainly Late Carboniferous-Permian) sequences and volcanism in the Balkans and Caucasus. It is possible to correlate lithological and facial carracteristics of the Up- per Palaeozoic sections in both of the regions, mainly for the continental, subaereal and shallow marine molasses from the Balkan Peninsula and Northern parts of the Caucasus, being the Fore-Range, Bechasin or Laba-Malka (the Northern slope of the Great Caucasus), Main Range, Southern slope of the Great Caucasus, Southern and Northern Transcaucasus. The comparable Upper Carboniferous and Permian sequences of the Caucasus and Balkans may be related to the Variscan orogeny and its neighbouring lowlands. The formation of the orogen was a result of the continent-continent collision between some peri-Gondwanan terranes and the southern periphery of the East-European platform. In the Caucasus, the continental and arc-related and oceanic ridges are also iden- tified. The distribution and relationships of the continental, transitional and shallow-marine facies in the eastern Balkans and Western Caucasian zones indicate the presence of a marine basin within the present-day Black sea during the Late Palaeozoic.
    [Show full text]
  • The Late Stage of Retreating Subduction in the Alpine-Mediterranean Region: Constraints from Travel Time Seismic Tomography
    PROBLEMS IN GEOPHYSICS FOR THE NEW MILLENNIUM Eds.Enzo Boschi, Göran Ekström and Andrea Morelli The late stage of retreating subduction in the Alpine-Mediterranean region: constraints from travel time seismic tomography ANDREA MORELLI and CLAUDIA PIROMALLO IStituto Nazionale di Geofisica, Roma, Italy A b s t r a c t - Seismological modelling of the upper mantle of the Africa-Eurasia colli- sion region has given images of its structure which can be used to supplement surface (geologic) information in the attempt to understand past and active tectonic process- es. A foremost feature of the region is given by the sinuous Alpine-Mediterranean thrust belt, under which subducted lithosphere is imaged by seismic tomography as seismically fast material (colder than ambient rock). Several arcuate structures are present, combining an external thrust front with an internal extensional basin, origi- nated by slab rollback: the Hellenic arc with the Aegean basin, the Calabrian arc with the Tyrrhenian Sea, the Betic-Rif with the Alboran Sea, and the Carpathians with the Pannonian basin. These systems are at different stages of their life, and all but the Hellenic-Aegean appear close to their terminal phase. Shape and extent of subducted slabs provide constraints on their evolution. Tomographic results, in all but the Hel- lenic-Aegean system, show a general lack of overall continuity of the subducted bod- ies, and in many cases support the idea that other processes, such as slab detachment or mantle delamination, contributed to shape the present day tectonics. Although to- mographic results have steadily improved image resolution with time, differences be- tween studies may lead to different interpretations.
    [Show full text]
  • Pre-Mesozoic Crimea As a Continuation of the Dobrogea
    International Journal of Earth Sciences https://doi.org/10.1007/s00531-019-01770-2 ORIGINAL PAPER Pre‑Mesozoic Crimea as a continuation of the Dobrogea platform: insights from detrital zircons in Upper Jurassic conglomerates, Mountainous Crimea N. B. Kuznetsov1,2,3 · E. A. Belousova2 · W. L. Grifn2 · S. Y. O’Reilly2 · T. V. Romanyuk2,4 · S. V. Rud’ko1 Received: 24 June 2019 / Accepted: 29 August 2019 © Geologische Vereinigung e.V. (GV) 2019 Abstract U–Pb dating, Hf-isotope, and trace-element studies on two detrital zircon samples from sandstone interlayers in the Upper Jurassic conglomerates of the Southern coast of the Mountainous Crimea provide new information on the primary crystalline complexes from which those conglomerates were sourced. The U–Pb age spectra of studied zircons suggest that they were most likely sourced from the (meta)sedimentary complexes of the Eastern and Western Pontides blocks and the Dobrogea platform. In particular, a close similarity of the Precambrian age spectra with the detrital zircons from Late Neoproterozoic– Late Paleozoic (meta)sedimentary complexes of the Dobrogea block provides strong supporting evidence for the afnity between the Pre-Mesozoic basement of the Crimea and the Dobrogea platform. The zircons in the frst sample were recycled through Dobrogea sedimentary complexes and originated from terranes with Amazonia afnities, while zircons in the sec- ond sample were recycled through the Taurides and originated from terranes related to northeastern Africa and Arabia. The strong similarity of the Precambrian parts of the age spectra of the Dobrogea complexes and the sample K15-007 suggests a resemblance of the Crimea’s Pre-Mesozoic foundation and the Dobrogea platform.
    [Show full text]
  • Geological Resource Analysis of Shale Gas and Shale Oil in Europe
    Draft Report for DG JRC in the Context of Contract JRC/PTT/2015/F.3/0027/NC "Development of shale gas and shale oil in Europe" European Unconventional Oil and Gas Assessment (EUOGA) Geological resource analysis of shale gas and shale oil in Europe Deliverable T4b mmmll Geological resource analysis of shale gas/oil in Europe June 2016 I 2 Geological resource analysis of shale gas/oil in Europe Table of Contents Table of Contents .............................................................................................. 3 Abstract ........................................................................................................... 6 Executive Summary ........................................................................................... 7 Introduction ...................................................................................................... 8 Item 4.1 Setup and distribute a template for uniformly describing EU shale plays to the National Geological Surveys .........................................................................12 Item 4.2 Elaborate and compile general and systematic descriptions of the shale plays from the NGS responses ....................................................................................15 T01, B02 - Norwegian-Danish-S. Sweden – Alum Shale .........................................16 T02 - Baltic Basin – Cambrian-Silurian Shales ......................................................22 T03 - South Lublin Basin, Narol Basin and Lviv-Volyn Basin – Lower Paleozoic Shales ......................................................................................................................37
    [Show full text]
  • Contribution to the Paleozoic Evolution of the Recent Moesian Platform
    GEOLOGICA BALCANICA, 25. 5·6, Sofia, Decemb. 1995, p. 3-21 Contribution to the Paleozoic evolution of the recent Moesian platform Slavcho Y anev, JUana Boncheva Geologica/Institute, Bulgarian Academy of Sciences, 1113 Sofia (Submitted: 11.04.1994; revised manuscript received and accepted 21.03.1995) C.RHetJ, H. IioH'IetJa - BIC.IIaiJ 6 naAeo3oiicKyiO 360AIOIIUIO cOtJpeMeHHou MuJuucKou IIAUmbl. - flll.lleO:JOiiCJCHe, H ):neUHIUibHO, CHJJypHitCJCHe H ,lle80HCJCHe, OTJJOJr;eHHll MH:JHiiCJCOil nJJHTbl xap1UCTepH3HpyJOTCll O'ieHb p83Hoo6p83HbiMH H 8 pll,lle CJJy'lae8 :JHa'IHTeJJbHbiMH HaJCJJOHaMH nJJaCT08 (oT 15-20" .ao 90"). B ~eepHax Ha6mo.aanHcb CJCJJB.IlJCH p83JIH'IHoro MacwTa6a. B oca.axax yCTaHOil.lleHbl nepepb18bl MeliCJlY Op.ll08HKOM H CHJJypoM (?), 8 HHJICHeM .aeBOHe, cpe.aHeM Jle80He (.118a), nepe.a HHli:HHM up6oHOM, nepe.a 8epxHeM 8H3ee, 8 HHJr;HeM xap6oHe (YpH), 8 8epxHeM xap6oHe ('teTwpe) H 8 nepMH (YpH). lbCTb p83MH808 JIHK8HJ1Hp081Ula nOJJHOCTbJO OTJleJJbHble cepHH H CHCTeMbl. TeJCTOHH'IeCICU DO,IlBHJr;HOCTb 06JJaCTH AOJCYMeHTHpyeTCll CHJJbHHMH . 8apHaUHJIMH MOIUHOCTeit 8 xap60He (OT 0 AO 3000 m), 8 nepMH (OT 0 AO 3500 m) H np. CllaUHIUibHble oco6eHHOCTH AOxyMeHTHpyJOT p83JIH'IHyJO rJJy6HHY H nOA8HJr;HOC AHO 8 AeBOHCJCHii nepHOA; np6oHaTHyJO DJJanpopMy- 8 BepXHHH YypH3 - · cpeAHHA 8H:Je; npH6peliCHHe OCB.IliCH- 8 BepXHHil 8H:Jee; noABOAHyJO AeJJbTy 8 HHJICHHH ~eap6oH H IUJJIJ08Hil.llbHyJO pa8HHHY- 8 sepXHHH xap6oH 8 Ao6py.11•e; npon108Hil.llbHble OCB.IlKH H KOHTHHeHTBJJbHblil 6acceHH (8VIJO'IBJI ce6XH B flpoBIUIHiiCJCOM pailOHe) - 8 DepMb • .6JJaro.aapeHHe 6HCTpOH H pe31COii CMeHbl 0JlH0803paCTHbiX ICOHO.IlOHTHbiX aCCOUHIUlHA H C DOMOIUbJO KOHOJlOHTHbiX MO,IleJJeii 6aTHMCYpH'IeCKOii npHypO'IeHHOCTH YCTaHOBJIHBaeTCll HIUJH'IHe CMeHbl a ceAHMeHTBUHOHHbiX o6cTaH08JCax OAHoro H roro •e CYpaTHrpaciiH'Iecxoro AHana:JOHa (cpeAHHil .aesoH - eiiljlenb).
    [Show full text]
  • General Overview of Geothermal Energy in Bulgaria, Klara Bojadgieva, Vladimir Hristov and Aleksey Benderev, Acta Montanistica
    Acta Montanistica Slovaca Ročník 12 (2007), mimoriadne číslo 1, 86-91 General overview of geothermal energy in Bulgaria Klara Bojadgieva1, Vladimir Hristov and Aleksey Benderev Všeobecný prehľad geotermálnej energie v Bulharsku Low enthalpy geothermal reservoirs have been discovered on the territory of Bulgaria. Most of the geothermal resource has been revealed. About 160 geothermal fields of totally 4600 l/s flow rate were explored. Currently application, hermal water is mainly in balneology, space heating, bottling of potable water and in swimming pools. The total installed capacity amounts to 109.7 MWt and the annual energy use is 1671.43 TJ/year. Major characteristics of geothermal fields have been summarized. Different types of application are discussed and the most perspective geothermal reservoirs selected in terms of their thermal capacity are listed. Key words: thermal water temperature, flow rate, thermal capacity, thermal water use Introduction The most intensive development of use of the thermal water and geothermal energy in Bulgaria took place in the period 1980 - 1990. Heating installations assisted by plate heat exchangers and heat pumps were constructed during this time. Social and economical changes in the last 15 years impeded the geothermal resource development. State investments have been sharply reduced. A new legislation on the water exploration, protection and application has been completed and tested. Only the bottling of mineral water and the soft drink preparation marked a rapid development in this period and the number of enterprises increased from 3 to 41. Several demonstration projects for space heating funded by international sources have been constructed. The renovation of spa resorts have started and many outdoor and indoor swimming pools were built.
    [Show full text]
  • SYMPOSIUM III: Geodynamic of the Alpine Orogen
    142 SYMPOSIUM III: GEODYNAMIC O THE ALPINE OROGEN INTEGRATED MODELLING AND RHEOLOGICAL STUDY O THE WESTERN CARPATHIANS M. BIELIK1, H. ZEYEN2 and A. LANKREIJER3 1Geophysical Institute of the Slovak Academy of Sciences, Dúbravská cesta 9, 842 28 Bratislava, Slovak Republic; [email protected] 2Department des Sciences de la Terre, Universite de Paris-Sud, Bat. 504, 9-91405 Orsay Cedex, 9rance 3Institute of Earth Sciences, Vrije Universiteit, 1081 HV Amsterdam, The Netherlands Key words: Integrated modelling, rheology, finite element algorithm, Western Carpathians. Introduction 9or the purpose of solving geological and geophysical problems in framework of the PANCARDI project we concentrated on the intergrated modelling of the geophysical fields. Alhough the West- ern Carpathians belong to the regions which are geophysically well surveyed, the study of its lithospheric structure has usually been performed by independent interpretation of the single geo- physical fields. Lateral and temporal changes in the lithosphere rheology of the Carpathian-Pannonian region have been shown to have pronounced effects on lithosphere dynamics (Lankreijer et al. 1996). Therefore rheological constraints on geodynamic models in the studied area are very important. Integrated modelling and rheological study of the Western Carpathian lithosphere was car- ried out along deep seismic reflection transect 2T. Methods ig. 1. Results of the integrated modelling along NNW-SSE Slovak Geotransect 2T. Explanations: (a) Surface heat flow. Commas represent The applied integrated modelling is capable of determining two- measured values with corresponding error bars. The solid line represents dimensional thermal lithospheric structure. On the basis of a finite calculated data. (b) Bouguer anomaly and (c) Elevation. Commas corre- element algorithm (Zeyen & 9ernandez 1994), the temperature spond to measured data and solid lines to calculated values.
    [Show full text]
  • Bulgaria, Romania, Ukraine) EIA/ARI World Shale Gas and Shale Oil Resource Assessment
    Technically Recoverable Shale Oil and Shale Gas Resources: Other Eastern Europe September 2015 Independent Statistics & Analysis U.S. Department of Energy www.eia.gov Washington, DC 20585 September 2015 This report was prepared by the U.S. Energy Information Administration (EIA), the statistical and analytical agency within the U.S. Department of Energy. By law, EIA’s data, analyses, and forecasts are independent of approval by any other officer or employee of the United States Government. The views in this report therefore should not be construed as representing those of the Department of Energy or other Federal agencies. U.S. Energy Information Administration | Technically Recoverable Shale Oil and Shale Gas Resources i September 2015 Contents Executive Summary ....................................................................................................................................... 3 Introduction ............................................................................................................................................. 3 Resource categories ................................................................................................................................. 3 Methodology ........................................................................................................................................... 5 Key exclusions .......................................................................................................................................... 6 Other Eastern Europe……………………………………
    [Show full text]
  • Plate Tectonic Aspects of the Triassic Carbonate-Hosted Stratiform
    www.geologia-croatica.hr Plate tectonic aspects of the Triassic carbonate-hosted stratiform-stratabound base-metal deposits in the Western Balkan, NW Bulgaria Irina Marinova* and Zhelyazko Damyanov Bulgarian Academy of Sciences, Institute of Mineralogy and Crystallography, Acad. G. Bonchev Str., Block 107, 1113 Sofia, Bulgaria (*corresponding author: [email protected]) 65-73 4 Figs. 2 Pls. doi: 10.4154/gc.2016.05 ABSTRACT Article history: The Triassic carbonate-hosted stratiform-stratabound base-metal deposits in the Western Received November 06, 2015 Balkan, NW Bulgaria, have well defined regional geological and tectonic settings, style of Revised and accepted December 09, 2015 mineralisation, mineralogical, geochemical and isotopic data. Their genesis, however, re- Avaliable online February 29, 2016 mains controversial in the framework of plate tectonic models, and is not supported by comparative analysis of possible counterpart candidates within the NW Tethyan domain. Besides, the crucial missing information is the geochronology of ore mineralisation relative to the Triassic carbonate host rocks. The article stresses the ambiguities due to the lack of mineralisation age dating, and emphasises the necessity for building a convincing plate tectonic model based on the relevant geodynamic setting. A prospective direction of re- Keywords: siderite-base metal deposits, search is the critical comparison with equivalent sediment-hosted base-metal deposits with- Kremikovtsi-Vratsa ore district, Triassic in the continental margin environments
    [Show full text]
  • The Metamorphic Basement of Romanian Carpathians: a Discussion of K-Ar and 40Ar/39Ar Ages
    Studia Universitatis Babeş-Bolyai, Geologia, 2006, 51 (1-2), 15 - 21 The metamorphic basement of Romanian Carpathians: a discussion of K-Ar and 40Ar/39Ar ages Carol STRUTINSKI1, Adrian PUŞTE2* & Rodica STAN3 1 Postfach 10 28 20, 66028 Saarbrücken, Germany 2 Department of Mineralogy, “Babeş-Bolyai” University, 1 Kogălniceanu, 400084 Cluj Napoca, Romania 3 Geological Institute of Romania, PO Box 181, 400084 Cluj Napoca, Romania Received June 2004; accepted July 2006 ABSTRACT. More than 600 radiometric K-Ar ages on rocks from the metamorphic basement of the Romanian Carpathians are statistically treated and discussed. The data suggest that the most pervasive Alpine rejuvenation occurred in a belt of about 100-120 km width, within which crystalline rocks were intensely reworked, undergoing a metamorphic remobilisation of Barrovian type before Middle – Late Cretaceous. This Eo-Alpine metamorphic belt outcrops on the flanks of the Mureş Zone, i.e., in the Rodna massif to the NE, and in the Northern Apuseni to the west. Away from it, ages get progressively older and outline a broad Variscan metamorphic province. In the most external part of the South Carpathians preserved pre-Variscan ages point to the former extension of the Moesian Plate. Within the study area radiometric K-Ar ages, as well as recently reported fission-track data, do not support reheating above 300°C and corresponding regional metamorphic events during meso- and neo-Alpine times. Key words: K-Ar dating, Alpine metamorphism, pre-Alpine metamorphism, Romania. 1. INTRODUCTION To avoid space problems in plotting, some individual In the last four decades of the past century, an ages coming from the same area/unit and having the same impressive number of K-Ar age determinations on characteristics (same age group and processed mineral) have metamorphic rocks from the basement of the Romanian been grouped together and are represented on the map by Carpathians were carried out, mainly at the only one symbol.
    [Show full text]