DOCSLIB.ORG

Implication of Mineralogy and Isotope Data on the Origin of the Permian Basic Volcanic Rocks of the Hronicum (Slovakia, Western Carpathians)

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Implication of Mineralogy and Isotope Data on the Origin of the Permian Basic Volcanic Rocks of the Hronicum (Slovakia, Western Carpathians) minerals Article Implication of Mineralogy and Isotope Data on the Origin of the Permian Basic Volcanic Rocks of the Hronicum (Slovakia, Western Carpathians) Ján Spišiak 1,* , Anna Vozárová 2, Jozef Vozár 3, Štefan Ferenc 1, Viera Šimonová 1 and Juraj Butek 1 1 Department of Geography and Geology, Faculty of Natural Sciences, Matej Bel University, Tajovského 40, SK-97401 Banská Bystrica, Slovakia; [email protected] (Š.F.); [email protected] (V.Š.); [email protected] (J.B.) 2 Department of Mineralogy and Petrology, Faculty of Natural Sciences, Comenius University, Mlynská Dolina, SK-84215 Bratislava, Slovakia; [email protected] 3 Earth Science Institute Slovak Academy of Science, Dúbravská cesta 9, SK-84005 Bratislava, Slovakia; [email protected] * Correspondence: [email protected] Abstract: The paper presents new geochemical data of the basic to intermediate volcanic rocks from the Hronic unit. The studied rocks are strongly altered and the primary mineral composition (clinopyroxenes, amphiboles, spinels, biotites, and plagioclases) is preserved only in some localities. The clinopyroxene corresponds to augite and primary amphiboles to pargasites. Spinels have a chemical composition similar to spinels from volcanic rocks. According to chemical composition, the studied basalts correspond to rift-related continental tholeiites. 143Nd/144Nd vs. 87Sr/86Sr isotopic 143 144 143 144 Citation: Spišiak, J.; Vozárová, A.; ratios of the basalts are scattered around the value of Nd/ Nd for CHUR, where Nd/ Nd 87 86 Vozár, J.; Ferenc, Š.; Šimonová, V.; ratios are relatively stable and Sr/ Sr values are relatively varied. According to isotopic ratio 207 204 206 204 Butek, J. Implication of Mineralogy of Pb/ Pb vs. Pb/ Pb, the basalt analyses lie in the field of EMII (mantle source enriched and Isotope Data on the Origin of the with crustal materials). The new results of U-Pb LA-ICP-MS dating of apatite point to an age Permian Basic Volcanic Rocks of the 254 ± 23 Ma (Lopingian). Hronicum (Slovakia, Western Carpathians). Minerals 2021, 11, 841. Keywords: Western Carpathians; Hronic Unit; Permian volcanic rocks; geochemistry; Sm/Nd and https://doi.org/10.3390/min11080841 Pb isotopes Academic Editors: Alexey V. Ivanov and Ivan Vlastélic 1. Introduction Received: 25 May 2021 Accepted: 28 July 2021 The Pennsylvanian–Permian continental sedimentary basin of the Hronicum repre- Published: 4 August 2021 sents a type of retroforeland basin [1,2], whose origin has been genetically associated with the convergent regime in the final stages of the Western Carpathian Variscan orogeny. Publisher’s Note: MDPI stays neutral This sedimentary basin is characterized by a huge amount of red-beds type siliciclastic with regard to jurisdictional claims in sediments accompanied by basic to intermediate volcanic rocks. Relics of the original filling published maps and institutional affil- of this sedimentation area are preserved in today’s Western Carpathian structure within a iations. system of superficial nappes, whereas they are completely tectonically detached from their original basement. The crustal character of the original basement was inferred from petro- logical analysis of sediments [3–5] as well as isotopic ages of clastic mica [6], monazite [7], and zircon [8]. The results documented an active continental margin crust provenance, Copyright: © 2021 by the authors. with dominant Devonian–Mississippian and Pennsylvanian magmatic sources. Licensee MDPI, Basel, Switzerland. This article studied basic to intermediate volcanic rocks whose genesis and chemical This article is an open access article composition are closely related to the tectonic processes that led to the formation of the distributed under the terms and Hronicum Pennsylvanian–Permian sedimentary realm. Previous analyses of the Hronicum conditions of the Creative Commons basalts/andesites have been focused on their field distribution and description of structural Attribution (CC BY) license (https:// relations and especially on their mineral and chemical composition [9–11]. They were creativecommons.org/licenses/by/ generally classified as rift-related continental tholeiites. 4.0/). Minerals 2021, 11, 841. https://doi.org/10.3390/min11080841 https://www.mdpi.com/journal/minerals Minerals 2021, 11, 841 2 of 28 In this paper, we briefly review the main characteristics of the Permian magmatism in the Hronic unit domain and present new chemical and isotopic data in an attempt to provide some insights into its origin and significance. The main goal of this study is to bring new petrological and geochemical data and identify in more detail the sources of magmas and differentiation processes, and thus infer the relationships with the geotectonic setting of the studied area. Therefore, nine additional samples were collected from the Hronicum Permian volcanic rocks for a better temporal covering of the Hronic formation (Table1). The studied samples were collected from the Permian volcanites of the 1st and 2nd eruption phases as well as from the dykes crossing Pennsylvanian sediments. Table 1. Location of samples. Sample GPS Rock Type Sample Locality No. Coordinates Malužinská dolina Valley, cliff 48◦57.1820 N M-1 coarse-grained gabbro-diorite dyke on the right slope of the forest 19◦48.7830 E road 812 m a.s.l. Malužinská dolina Valley, cliff 48◦57.1820 N M-1A fine-grained gabbro-diorite dyke on the right slope of the forest 19◦48.7830 E road 812 m a.s.l. Hodruša Valley, SE from the Malužiná Village, cliff on the 48◦57.5520 N M-2 andesite/basalt-2nd eruption phase right slope of the forest road, 19◦50.0510 E 870m a.s.l. Malužinská dolina Valley, 48◦57.5440 N M-3 andesite/basalt-2nd eruption phase forest road cut, 1.4 km SE from 19◦50.0910 E Malužiná Village, 770 m a.s.l. N from the Liptovská Tepliˇcka Village, abandoned quarry 48◦59.0380 N M-4 andesite/basalt-1st eruption phase along the Šuˇnava-Liptovská 20◦05.3530 E Tepliˇckaroad, 890 m a.s.l. Benkovský potok Valley, small 49◦00.4680 N M-5 basaltic andesite-1st eruption phase quarry at the left side of the 19◦59.7470 E forest road, 832 m a.s.l. S from the Hranovnica Village, forest road at the left slope of 48◦57.9700 N M-7 basaltic andesite-1st eruption phase the Vernár-Hranovnica state 20◦17.5660 E road, 694 m a.s.l. West end of the Nižná Boca 48◦56.9150 N M-8 coarse-grained gabbro-diorite dyke Village, 860 m a.s.l. 19◦46.1570 E 49◦00.5210 N M-9 andesite/basalt-2nd eruption phase Kvetnica quarry, 725 m a.s.l. 20◦17.0850 E 2. Geological Background The Hronic nappe system (Figure1) structurally represents the highest tectonic unit in the Central Western Carpathians. There is no generally accepted opinion about the structure and composition of the Hronic nappe system and its palaeogeographic position. A lot of theories have emerged in the past four decades of research, with current defini- tion of Hronicum as a rootless superficial nappe system [12,13] that mostly comprises a Carboniferous–Permian volcano-sedimentary sequence and Triassic carbonate sediments (with significant similarities of the latter to the Oberostalpine-type). Jurassic-Lower Creta- ceous sediments are preserved only locally [14]. Minerals 2021, 11, 841 3 of 28 Minerals 2021, 11, x FOR PEER REVIEW 3 of 27 Figure 1. SimplifiedFigure 1. geologicalSimplified sketchgeological map sketch of the map Western of the Carpathians Western Carpathians [15] and schematic [15] and geologicalschematic mapgeological of the Hronicum map of the Hronicum Pennsylvanian–Permian sequence on the northern slopes of the Nízke Tatry Pennsylvanian–Permian sequence on the northern slopes of the Nízke Tatry Mts. showing sample locations [15]. Mts. showing sample locations [15]. The allochthonous position of Hronicum superficial nappes relative to basement The allochthonousimplies an position ultra-Veporic of Hronicum origin. superficial Hronicum nappes probably relative comes to frombasement the area im- that originally plies an ultra-Veporicexisted betweenorigin. Hronicum the Veporicum probab andly comes Gemericum from the units area [16 that–18 ].originally The southernmost ex- tectonic isted between occurrencesthe Veporicum of Hronic and Gemericum debris were units recognized [16–18]. along The thesouthernmost line Luben ítectonick–Margecany (tectonic occurrences of contactHronic Veporicum/Gemericum).debris were recognized along Generally, the line the HronicumLubeník–Margecany nappes rest (tec- directly on the Fa- tonic contact Veporicum/Gemericum).tricum unit, except for Veporicum Generally, zone the whereHronicum Hronicum nappes directly rest directly overthrust on the crystalline the Fatricum unit,complex except of Veporicumfor Veporicum [19]. zone where Hronicum directly overthrust the crystalline complex Theof Veporicum original basement [19]. of the Hronicum is currently undetermined. The character of The originalthe basement Pennsylvania–Permian of the Hronicum terrestrial is currently siliciclastic undetermined. sediments The suggests character that of they originated the Pennsylvania–Permianfrom a sedimentary terrestrial basin siliciclastic located onsediments the continental suggests crust. that Thisthey opinionoriginated is also supported from a sedimentaryby findings basin located of some on mylonitized the continental granitoid crust. tectonic This opinion slices belowis also the supported basal part of the lower by findings of somepartial mylonitized Hronicum nappegranitoid [20 ,tectonic21]. The slices age of below the source the basal area part (310–340 of the Ma)lower was determined partial
Load more

Recommended publications
  • Southward-Directed Subduction of the Farallon–Aluk Spreading Ridge and Its Impact on Subduction Mechanics and Andean Arc Magmatism: Insights From
    feart-08-00121 May 7, 2020 Time: 11:30 # 1 ORIGINAL RESEARCH published: 08 May 2020 doi: 10.3389/feart.2020.00121 Southward-Directed Subduction of the Farallon–Aluk Spreading Ridge and Its Impact on Subduction Mechanics and Andean Arc Magmatism: Insights From Edited by: Marina Manea, Geochemical and Seismic National Autonomous University of Mexico, Mexico Tomographic Data Reviewed by: 1,2 1,2 1,2 1,2 Luca Ferrari, Sofía B. Iannelli *, Lucía Fernández Paz , Vanesa D. Litvak , Guido Gianni , Geosciences Center, National Lucas M. Fennell1,2, Javiera González3, Friedrich Lucassen4, Simone Kasemann4, Autonomous University of Mexico, Verónica Oliveros3 and Andrés Folguera1,2 Mexico 1 2 Jiashun Hu, Departamento de Ciencias Geológicas, Universidad de Buenos Aires, Buenos Aires, Argentina, Instituto de Estudios 3 California Institute of Technology, Andinos ‘Don Pablo Groeber’, CONICET- Universidad de Buenos Aires, Buenos Aires, Argentina, Departamento 4 United States de Ciencias de la Tierra, Universidad de Concepción, Concepción, Chile, MARUM - Center for Marine Environmental Sciences and Faculty of Geosciences, University of Bremen, Bremen, Germany *Correspondence: Sofía B. Iannelli sofi[email protected] Since the initial proposal of the past existence of a southward-directed mid-ocean ridge–subduction interaction in the Andes during Late Cretaceous–Paleogene times, Specialty section: This article was submitted to several studies have been devoted to uncover the tectonomagmatic evidence of this Structural Geology and Tectonics, process. The collision of a spreading ridge against a subduction margin provokes a section of the journal important tectonomagmatic changes, including, between them, variations in arc-related Frontiers in Earth Science magmatic activity and in the plate-margin stress regime.
    [Show full text]
  • And Ordovician (Sardic) Felsic Magmatic Events in South-Western Europe: Underplating of Hot Mafic Magmas Linked to the Opening of the Rheic Ocean
    Solid Earth, 11, 2377–2409, 2020 https://doi.org/10.5194/se-11-2377-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Comparative geochemical study on Furongian–earliest Ordovician (Toledanian) and Ordovician (Sardic) felsic magmatic events in south-western Europe: underplating of hot mafic magmas linked to the opening of the Rheic Ocean J. Javier Álvaro1, Teresa Sánchez-García2, Claudia Puddu3, Josep Maria Casas4, Alejandro Díez-Montes5, Montserrat Liesa6, and Giacomo Oggiano7 1Instituto de Geociencias (CSIC-UCM), Dr. Severo Ochoa 7, 28040 Madrid, Spain 2Instituto Geológico y Minero de España, Ríos Rosas 23, 28003 Madrid, Spain 3Dpt. Ciencias de la Tierra, Universidad de Zaragoza, 50009 Zaragoza, Spain 4Dpt. de Dinàmica de la Terra i de l’Oceà, Universitat de Barcelona, Martí Franquès s/n, 08028 Barcelona, Spain 5Instituto Geológico y Minero de España, Plaza de la Constitución 1, 37001 Salamanca, Spain 6Dpt. de Mineralogia, Petrologia i Geologia aplicada, Universitat de Barcelona, Martí Franquès s/n, 08028 Barcelona, Spain 7Dipartimento di Scienze della Natura e del Territorio, 07100 Sassari, Italy Correspondence: J. Javier Álvaro ([email protected]) Received: 1 April 2020 – Discussion started: 20 April 2020 Revised: 14 October 2020 – Accepted: 19 October 2020 – Published: 11 December 2020 Abstract. A geochemical comparison of early Palaeo- neither metamorphism nor penetrative deformation; on the zoic felsic magmatic episodes throughout the south- contrary, their unconformities are associated with foliation- western European margin of Gondwana is made and in- free open folds subsequently affected by the Variscan defor- cludes (i) Furongian–Early Ordovician (Toledanian) activ- mation.
    [Show full text]
  • Masterarbeit
    MASTERARBEIT Titel der Masterarbeit Late Cretaceous Volcaniclastic Rocks in the Pontides (NW Turkey) verfasst von Katharina Böhm BSc angestrebter akademischer Grad Master of Science (M.Sc.) Wien, 2015 Studienkennzahl lt. Studienblatt: A 066 815 Studienrichtung lt. Studienblatt: Erdwissenschaften Betreuerin / Betreuer: Ao. Univ.-Prof. Dr. Michael Wagreich Declaration ”I hereby declare that this master’s thesis was authored by myself independently, without use of other sources than indicated. I have explicitly cited all material which has been quoted either literally or by content from the used sources. Further this work was neither submitted in Austria nor abroad for any degree or examination.” Contents Declaration2 1. Introduction8 1.1. Project.................................. 9 1.1.1. Goals............................... 9 1.2. Geographical setting.......................... 10 1.3. Geological setting............................ 12 1.3.1. The Pontides........................... 14 1.3.2. The Pontides in the Cretaceous................ 18 1.3.3. Correlation with relative ages.................. 24 2. Nomenclature 28 3. Methods 29 3.1. ICP-ES and ICP-MS........................... 29 3.2. PXRD.................................. 29 3.3. Heavy mineral extraction........................ 30 4. Results 31 4.1. Mineralogy................................ 31 4.1.1. Powder X-Ray diffraction.................... 31 4.1.2. Thin sections.......................... 33 4.1.3. Mineral Extraction: Dating of minerals............. 34 4.2. Geochemistry.............................. 36 5. Interpretation of the geochemical results 37 5.1. Mobility of elements........................... 37 5.2. Alteration of minerals.......................... 39 5.3. Determining the rock type........................ 41 3 5.4. Discriminating volcanic series..................... 48 5.5. Revealing the tectonic setting...................... 52 5.6. Plotting geochemical element patterns................. 60 5.7. Summary of the geochemical classification.............. 62 6.
    [Show full text]
  • Vulcanitas Alcalinas En El Sector Del Cerro Morado, Departamento
    CARACTERÍSTICAS GEOQUÍMICAS DE LAS VULCANITAS ALCALINAS CRETÁCICAS EN EL SECTOR DEL CERRO MORADO, DEPARTAMENTO JÁCHAL, SAN JUAN, ARGENTINA. S. Pérez Luján Departamento de Geología. Facultad de Ciencias Exactas, Físicas y Naturales. Universidad Nacional de San Juan. E-mail: [email protected] RESUMEN Rocas volcánicas alcalinas afloran en las cercanías del cerro Morado, en la terminación austral de la sierra de Mogna, en el borde oriental de Precordillera de San Juan. El estudio petrográfico y geoquímico de las manifestaciones volcánicas permitió clasificarlas como tefritas basaníticas o basanitas nefelínicas, con fuerte afinidad alcalina, mostrando una composición química característica de ambiente geotectónico de intraplaca. Las dataciones radimétricas, método K-Ar, con promedio de 90 ± 8 m.a. de antigüedad (Cingolani et al. 1984) indican una edad cretácica superior parte baja, para estas rocas. Los resultados obtenidos destacan el control geotectónico para el emplazamiento de las vulcanitas durante este periodo y su relación con otros asomos en otras localidades del centro y noroeste de argentino, que ha permitido a otros autores postular la existencia de una provincia petrográfica alcalina. Palabras clave: alcalinas, rocas volcánicas, Cretácico, intra placa ABSTRACT This paper deals with alkaline volcanic rocks that crop out at the Morado hill located in the southern end of the Mogna ranges, which are part of the Eastern border of the Precordillera in the San Juan province, Argentina. The petrography and geochemistry study of the alkaline volcanics has allowed to classify them as tephrite basanite or basanite nephelinite, with strong alkaline chemical affinity, showing a characteristic composition of within plate geochemistry environment. The radimetric analysis, K-Ar data, has shown an average 90 ± 8 m.y.
    [Show full text]
  • The Cretaceous Igneous Rocks in Southeastern Guangxi and Their Implication for Tectonic Environment in Southwestern South China Block
    Open Geosciences 2020; 12: 518–531 Research Article Yang Liu, Nianqiao Fang*, Menglin Qiang, Lei Jia, and Chaojie Song The Cretaceous igneous rocks in southeastern Guangxi and their implication for tectonic environment in southwestern South China Block https://doi.org/10.1515/geo-2020-0160 Keywords: high-magnesian andesites 1, I-type granite 2, received January 9, 2020; accepted May 13, 2020 clastoporphyritic lava 3, Neo-Tethyan Subduction 4, Abstract: Southeastern Guangxi is located in the south- Southwestern South China Block 5 western South China Block and to the northwest of the South China Sea (SCS), with abundant records of the Cretaceous magmatism. A detailed study of igneous rocks will contribute to a better understanding of the late 1 Introduction Mesozoic tectonic environment. Zircon U–Pb dating yields ages of 93.37 ± 0.43 Ma for Yulin andesites and 107.6 ± South China Block lies between the Tethyan tectonic belt fi [ ] 1.2 Ma for Luchuan granites. Yulin andesites are hornblende and Paci c tectonic belt 1 .Itisacrucialperiodfor andesites, of which w(MgO) is between 7.72% and 8.42%, magmatic rocks and mineralization in southwestern South and Mg# is between 66.7 and 68.0, belonging to high China Block in Cretaceous, especially in the range of – [ ] magnesian andesites (HMAs) from peridotite sources. 100 90 Ma 2 . These magmatic rocks are a key to study Luchuan granites are medium- to fine-grained monzogra- the tectonic evolution in this region. More research has - nites. Monzogranites and clastoporphyritic lava are high-K been done by predecessors, including Kunlunguan bath calc-alkaline series and metaluminum to weakly peralumi- olith, Dali rock mass and Dachang dike group with nous series, which belong to the I-type granites.
    [Show full text]
  • Ammonoid Genus Argentiniceras from Kachchh (India) and Its Relevance to J Urassic/Cretaceous Boundary
    Newsl. Stratigr. Berlin · Stuttgart, 28. 3. 1991 Discovery of Lower Berriasian (Lower Creataceous) Ammonoid Genus Argentiniceras from Kachchh (India) and its Relevance to J urassic/Cretaceous Boundary by jAr KRISHNA with 1 plate, 2 figures and 4 tables Abstract. The ammonoid genus Argentiniceras SPATH 1924 (= Andesites GERTH 1925) is described and illustrated from Umia Member (Green Oolitic bed) North of Lakhapar, Western Kachchh, Gujarat. The genus Argentiniceras is a Lower Berriasian form known so far only from South America (Colombia, Peru, Chile, Argentina) and Antarctica (Alexander Island) i.e. the Andean marine fauna! province (also known as S. American or SE Pacific) and it is considered a good marker of Lower Berriasian. This is the first report of this genus from anywhere outside the Andean Province. Its discovery in Jurassic/Cretaceous passage beds helps more precise and better delineation of the Jurassic/Cretaceous boundary in Kachchh. Further, together with the earlier reports of some South American Upper Tithonian genera from India, the present discovery also strengthens the evidence of direct marine connection between Andean and Indo-East-African marine fauna! provinces near the Jurassic/Cretaceous boundary. Resume. Le genre Argentiniceras SPATH 1924 (= Andesites GERTH 1925) decouvert clans le membre Umia (couche oolithique verte) au Nord de Lakhapar (Gujarat, Ouest de l'Inde) est decrit et illustre. D'age Berriasien inferieur, il etait connu jusqu'a present uniquement du Sud de l'Amerique (Colombie, Perou, Chili, Argentine) et de l'Antarctique (Ile Alexander), c'est-a-dire de la province andine. Le genre est considere comme un bon marqueur stratigraphique du Berriasien inferieur et pour la premiere fois est cite en-dehors de la province andine, clans les couches de passage Jurassique-Cretace.
    [Show full text]
  • New Age Constraints for Early Paleogene Strata of Central Patagonia
    New age constraints for early Paleogene strata of central Patagonia, Argentina New age constraints for early Paleogene strata of central Patagonia, Argentina: Implications for the timing of South American Land Mammal Ages J. Marcelo Krause1,2,†, William C. Clyde3, Mauricio Ibañez-Mejía4,5, Mark D. Schmitz6, Timothy Barnum3, Eduardo S. Bellosi7, and Peter Wilf8 1CONICET–Museo Paleontológico Egidio Feruglio, Avenida Fontana 140, 9100, Trelew, Argentina 2Departamento de Geología, Universidad Nacional de la Patagonia San Juan Bosco, Ruta Provincial 1 s/n, 9000, Comodoro Rivadavia, Chubut, Argentina 3Department of Earth Sciences, University of New Hampshire, 56 College Road, Durham, New Hampshire 03824, USA 4Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139, USA 5Department of Earth and Environmental Sciences, University of Rochester, Rochester, New York 14627, USA 6Department of Geosciences, Boise State University, 1910 University Drive, Boise, Idaho 83725, USA 7CONICET–Museo Argentino de Ciencias Naturales, Ángel Gallardo 470, 1405 Buenos Aires, Argentina 8Department of Geosciences, Pennsylvania State University, University Park, Pennsylvania 16802, USA ABSTRACT in our new magnetostratigraphic framework, rec ords of regional biotic responses to global we correlate the Peñas Coloradas Formation climatic events (e.g., Raigemborn et al., 2009, The Río Chico Group in the San Jorge to chrons C27n-26r (ca. 62.5 to ca. 61.6 Ma; 2014; Bellosi and González, 2010; Krause et al., Basin of central Patagonia (Argentina) pre- late Danian) and the section from the middle 2010; Dunn et al., 2015; Kohn et al., 2015; serves some of South America’s most signif- Las Flores to the uppermost Koluel-Kaike to Selkin et al., 2015).
    [Show full text]
  • (Turkey) Based on New Nannoplankton Age Determinations in the Eastern Pontides: Geodynamic Implications Jean-Claude Hippolyte, C
    Stratigraphic comparisons along the Pontides (Turkey) based on new nannoplankton age determinations in the Eastern Pontides: geodynamic implications Jean-Claude Hippolyte, C. Müller, E. Sangu, N. Kaymakci To cite this version: Jean-Claude Hippolyte, C. Müller, E. Sangu, N. Kaymakci. Stratigraphic comparisons along the Pontides (Turkey) based on new nannoplankton age determinations in the Eastern Pontides: geo- dynamic implications. The Geological Society, London, Special Publications, Geological Society of London, 2017, Tectonic Evolution of the Eastern Black Sea and Caucasus., 428 (1), pp.323 - 358. 10.1144/SP428.9. hal-01708711 HAL Id: hal-01708711 https://hal.archives-ouvertes.fr/hal-01708711 Submitted on 14 Feb 2018 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Copyright 1 Stratigraphic comparisons along the Pontides (Turkey) based on new nannoplankton age determinations in the Eastern Pontides: geodynamic implications J-C. Hippolyte, C. Müller, E. Sangu and N. Kaymakci Hippolyte Jean-Claude * UMR-6635 CNRS - Universite Aix-Marseille III BP 80, Europole Mediterraneen de l'Arbois 13545 Aix en Provence Cedex 4, FRANCE Tel. +33 4 42 97 17 70, Fax. +33 4 42 97 16 58, e-mail: [email protected] Müller Carla PL-66-431b Santok, Ludzislawice 36, Poland Sangu Ercan Kocaeli University, Department of Geological Engineering, 41100 Kocaeli, Turkey Kaymakci Nuretdın Middle East Technical University, Department of Geological Engineering, 06800- Ankara Turkey.
    [Show full text]
  • Remarkable Variability of Dyke Features at the Vicuña Pampa
    Remarkable variability of dyke features at the Vicuña Pampa Volcanic Complex, Southern Central Andes Silvina Guzmán, Marco Neri, Roberto Carniel, Joan Martí, Pablo Grosse, Carolina Montero-López, Adelina Geyer To cite this version: Silvina Guzmán, Marco Neri, Roberto Carniel, Joan Martí, Pablo Grosse, et al.. Remarkable variabil- ity of dyke features at the Vicuña Pampa Volcanic Complex, Southern Central Andes. Terra Nova, Wiley-Blackwell, 2017, 29 (4), pp.224-232. 10.1111/ter.12268. insu-01522829 HAL Id: insu-01522829 https://hal-insu.archives-ouvertes.fr/insu-01522829 Submitted on 15 May 2017 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Distributed under a Creative Commons Attribution - NonCommercial - NoDerivatives| 4.0 International License DR. SILVINA GUZMAN (Orcid ID : 0000-0003-3632-2960) DR. MARCO NERI (Orcid ID : 0000-0002-5890-3398) DR. CAROLINA MONTERO-LÓPEZ (Orcid ID : 0000-0002-3943-5648) Article type : Paper Reference number: TER-2016-0055.R2 Received date: 17-May-2016 Revised version received date: 31-Mar-2017 Accepted date: 06-Apr-2017
    [Show full text]
  • Petrogenesis of the Early Cretaceous Adakite-Like Porphyries And
    See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/257553072 Petrogenesis of the Early Cretaceous adakite- like porphyries and associated basaltic andesites in the eastern Jiangnan orogen... Article in Journal of Asian Earth Sciences · November 2012 DOI: 10.1016/j.jseaes.2012.10.017 CITATIONS READS 13 97 5 authors, including: Xiao-Lei Wang Ming Tang Nanjing University Rice University 49 PUBLICATIONS 1,467 CITATIONS 13 PUBLICATIONS 168 CITATIONS SEE PROFILE SEE PROFILE R. M. Gaschnig University of Massachusetts Lowell 34 PUBLICATIONS 293 CITATIONS SEE PROFILE All content following this page was uploaded by Ming Tang on 20 February 2014. The user has requested enhancement of the downloaded file. Journal of Asian Earth Sciences 61 (2012) 243–256 Contents lists available at SciVerse ScienceDirect Journal of Asian Earth Sciences journal homepage: www.elsevier.com/locate/jseaes Petrogenesis of the Early Cretaceous adakite-like porphyries and associated basaltic andesites in the eastern Jiangnan orogen, southern China ⇑ Xiao-Lei Wang a, , Xu-Jie Shu a, Xisheng Xu a, Ming Tang a, Richard Gaschnig b a State Key Laboratory for Mineral Deposits Research, Department of Earth Sciences, Nanjing University, Nanjing 210093, PR China b Department of Geology, University of Maryland, MD 20742, USA article info abstract Article history: Early Cretaceous quartz porphyries are associated with mantle-derived mafic rocks (basaltic andesites) in Received 4 October 2011 the eastern segment of the Neoproterozoic Jiangnan orogen, southern China. Zircons from two quartz Received in revised form 10 October 2012 porphyries yield identical U–Pb ages at 142 ± 1 Ma by the LA–ICP–MS method.
    [Show full text]
  • Hidrovolcanismo Parásito Asociado Al Volcán Diamante, Provincia De Mendoza
    Tesis de Grado Hidrovolcanismo parásito asociado al Volcán Diamante, Provincia de Mendoza Hense, Erich 2017 Este documento forma parte de las colecciones digitales de la Biblioteca Central Dr. Luis Federico Leloir, disponible en bibliotecadigital.exactas.uba.ar. Su utilización debe ser acompañada por la cita bibliográfica con reconocimiento de la fuente. This document is part of the digital collection of the Central Library Dr. Luis Federico Leloir, available in bibliotecadigital.exactas.uba.ar. It should be used accompanied by the corresponding citation acknowledging the source. Cita tipo APA: Hense, Erich. (2017). Hidrovolcanismo parásito asociado al Volcán Diamante, Provincia de Mendoza. Facultad de Ciencias Exactas y Naturales. Universidad de Buenos Aires. https://hdl.handle.net/20.500.12110/seminario_nGEO001102_Hense Cita tipo Chicago: Hense, Erich. "Hidrovolcanismo parásito asociado al Volcán Diamante, Provincia de Mendoza". Facultad de Ciencias Exactas y Naturales. Universidad de Buenos Aires. 2017. https://hdl.handle.net/20.500.12110/seminario_nGEO001102_Hense Dirección: Biblioteca Central Dr. Luis F. Leloir, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires. Contacto: bibliotecadigital.exactas.uba.ar Intendente Güiraldes 2160 - C1428EGA - Tel. (++54 +11) 4789-9293 Hidrovolcanismo parásito asociado al Volcán Diamante, Provincia de Mendoza Trabajo Final de Licenciatura Erich Hense Directora: Corina Risso -2017- Hidrovolcanismo parásito asociado al Volcán Diamante 2017 Índice 1. Resumen 3 2. Introducción 4 2.1. Objetivo 4 2.2. Metodología 4 2.3 Antecedentes 5 3. Características generales del área de estudio 6 3.1. Ubicación y vías de acceso 6 3.2. Contexto geográfico 7 3.3. Flora y fauna 8 3.4. Clima 9 4. Contexto Tectónico Regional 10 4.1.
    [Show full text]
  • Abstract Template for the Lasi Iii Conference
    Geoscience Society of New Zealand Miscellaneous Publication 131A Cerro Chivo Laguna Azul Abstract Volume of the Laguna Potrok Aike Fourth International Maar Conference 3IMC - ARGENTINA A Multidisciplinary Congress on Monogenetic Volcanism Edited by Kate Arentsen, Károly Németh, Elaine Smid Badacsony Tihany Filakovo 2IMC - HUNGARY - SLOVAKIA -GERMANY Pulvermaar Dauner Maare Auckland, New Zealand 20-24 February 2012 Eichholzmaar 1IMC - GERMANY Fourth International Maar Conference a multidisciplinary congress on monogenetic volcanism Auckland, New Zealand 20 – 24 February 2012 ABSTRACTS VOLUME Edited by Kate Arentsen, Károly Németh, Elaine Smid Geoscience Society of New Zealand Miscellaneous Publication 131A ISBN 978-1-877480-15-7 ISSN Online 2230-4495 ISSN Print 2230-4487 Previous IMCs International Maar Conference Daun, Germany, 2000 Second International Maar Conference Lajosmizse, Hungary, 2004 Third International Maar Conference Malargüe, Argentina, 2009 Conference Supporters International Association of Volcanology and Chemistry of the Earth’s Interior International Association of Sedimentologists Geoscience Society of New Zealand The University of Auckland Massey University Institute of Earth Science and Engineering Earthquake Commission Elsevier Springer Villa Maria Estate Epic Beer Organizing Committee Károly Németh and Ian EM Smith (Co-Chairs) Members: Kate Arentsen, Shane Cronin, Jan Lindsay, Janet Simes, Elaine Smid Scientific Advisory Group Georg Buechel, Kathy Cashman, Shane Cronin, Gonca Gençalioğlu Kuşcu, Guido Giordano, Stephan Kurszlaukis, Jan Lindsay, Volker Lorenz, Joan Marti, Károly Németh, Corina Risso, Hetu Sheth, Claus Siebe, Ian EM Smith, Young Kwan Sohn, Greg Valentine, James White, Bernd Zimanowski, Bernd Zolitschka IAVCEI – CMV/CVS – IAS 4IMC Conference Auckland, New Zealand, 2012 Preface We extend our warmest welcome to delegates of the Fourth International Maar Conference (4IMC) and look forward to hosting you in Auckland, New Zealand.
    [Show full text]