Relevant bibliographies by topics / Monzodiorite

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  1. Journal articles
  2. Dissertations / Theses
  3. Conference papers

Academic literature on the topic 'Monzodiorite'

Author: Grafiati
Published: 4 June 2021
Last updated: 1 February 2022

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Journal articles on the topic "Monzodiorite"

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Shin, Youngjae, Seungwook Shin, Seong-Jun Cho, and Jeong-Sul Son. "Application of 3D Electrical Resistivity Tomography in the Yeoncheon Titanomagnetite Deposit, South Korea." Minerals 11, no. 6 (2021): 563. http://dx.doi.org/10.3390/min11060563.

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The Yeoncheon titanomagnetite deposit formed by Precambrian magma differentiation is located in Gyeonggi-do, South Korea. Our team conducted an airborne magnetic survey for multiscale mineral exploration and then selected a promising survey area. An electrical resistivity survey was carried out in the potential area to image subsurface structure. Because ore minerals are mainly distributed in gabbro monzodiorite rather than quartz monzodiorite, we applied three-dimensional inversion of electrical resistivity tomography (ERT) data to identify lithology boundaries related to magma differentiatio
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Ávila, Ciro A., Wilson Teixeira, Umberto G. Cordani, et al. "The Glória quartz-monzodiorite: isotopic and chemical evidence of arc-related magmatism in the central part of the Paleoproterozoic Mineiro belt, Minas Gerais State, Brazil." Anais da Academia Brasileira de Ciências 78, no. 3 (2006): 543–56. http://dx.doi.org/10.1590/s0001-37652006000300013.

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The Glória quartz-monzodiorite, one of the mafic plutons of the Paleoproterozoic Mineiro belt, is intrusive into banded gneisses, amphibolites, schists and phyllites of the Rio das Mortes greenstone belt, in the southern portion of the São Francisco Craton, State of Minas Gerais, Brazil. The Glória quartz-monzodiorite yields a SHRIMP U-Pb zircon age of 2188 ± 29 Ma, suggesting a tectonic relationship with the pre-collisional phase of the Mineiro belt. According to the Nd isotopic evidence (epsilonNd(T) = -3.4; T DM = 2.68 Ga) the original magmas was formed by a mixture among Archean crustal ma
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Marincea, Ştefan, Delia-Georgeta Dumitraş, Cristina Sava, Frédéric Hatert, and Fabrice Dal Bo. "Mineralogy of a High-Temperature Skarn, in High CO2 Activity Conditions: The Occurrence from Măgureaua Vaţei (Metaliferi Massif, Apuseni Mountains, Romania)." Minerals 10, no. 8 (2020): 677. http://dx.doi.org/10.3390/min10080677.

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A shallow-level monzodioritic to quartz-monzodioritic pluton of the Upper Cretaceous age caused contact metamorphism of Tithonic–Kimmeridgian reef limestones at Măgureaua Vaţei (Metaliferi Massif, Apuseni Mountains, Romania). The preserved peak metamorphic assemblage includes gehlenite (Ak 33.64–38.13), monticellite, wollastonite-2M, Ti-poor calcic garnet, and Ca-Tschermak diopside (with up to 11.15 mol.% Ca-Tschermak molecule). From the monzodioritic body to the calcitic marble, the periplutonic zoning can be described as: monzodiorite/agpaitic syenite-like inner endoskarn/wollastonite + pero
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Tran, Hung Phu, and Vy Nguyen Hung Trinh. "U – Pb ISOTOPIC AGE IN ZIRCON OF THE GRANITOID ROCKS AT CAM MOUNTAIN – ANGIANG PROVINCE." Science and Technology Development Journal 14, no. 4 (2011): 46–56. http://dx.doi.org/10.32508/stdj.v14i4.2026.

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Results of analyzing U – Pb isotopic age for zircon in biotite granite, fine granite, monzodiorite, syenite diorite are 88±1,7 Ma, 86±1,7 Ma, 108±0,63 Ma 101±1,5 Ma,. These confirmed that they are Cretaceous age. Through this paper, many thanks to Professor Tony Crawford and Master Dinh Quang Sang (Tasmania University, Australia) for helping us to analyze these isotopic samples.
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STEINITZ, ADAR, YARON KATZIR, JOHN W. VALLEY, YARON BE'ERI-SHLEVIN, and MICHAEL J. SPICUZZA. "The origin, cooling and alteration of A-type granites in southern Israel (northernmost Arabian–Nubian shield): a multi-mineral oxygen isotope study." Geological Magazine 146, no. 2 (2008): 276–90. http://dx.doi.org/10.1017/s0016756808005566.

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AbstractA multi-mineral oxygen isotope study sheds light on the origin, cooling and alteration of Late Neoproterozoic A-type granites in the Arabian–Nubian shield of southern Israel. The oxygen isotope ratio of zircon of the Timna monzodiorite, quartz syenite and alkaline granite are within the range of mantle zircon (δ18O(Zrn) = 5.3 ± 0.6‰, 2σ), supporting the co-genetic mantle-derived origin previously suggested based on geochemical data and similar ɛNd(T) values and U–Pb ages (610 Ma). Likewise, olivine norite xenoliths within the monzodiorite (δ18O(Ol) = 5.41 ± 0.07‰) may have formed as cu
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Zhimulev, F. I., Yu A. Kalinin, V. P. Sukhorukov, et al. "Age of the Raygorodok Au-bearing Gabbro—Monzodiorite Massif (Northern Kazakhstan)." Doklady Earth Sciences 481, no. 2 (2018): 1033–36. http://dx.doi.org/10.1134/s1028334x18080238.

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Vander Auwera, J., J. Longhi, and J. C. Duchesne. "A Liquid Line of Descent of the Jotunite (Hypersthene Monzodiorite) Suite." Journal of Petrology 39, no. 3 (1998): 439–68. http://dx.doi.org/10.1093/petroj/39.3.439.

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KORONEOS, A., G. POLI, V. CVETKOVIĆ, G. CHRISTOFIDES, D. KRSTIĆ, and Z. PÉCSKAY. "Petrogenetic and tectonic inferences from the study of the Mt Cer pluton (West Serbia)." Geological Magazine 148, no. 1 (2010): 89–111. http://dx.doi.org/10.1017/s0016756810000476.

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AbstractThe Mt Cer Pluton, Serbia, is a complex laccolith-like intrusion (~ 60 km2), situated along the junction between the southern Pannonian Basin and northern Dinarides. It intrudes Palaeozoic metamorphic rocks causing weak to strong thermal effects. Based on modal and chemical compositions, four rock-types can be distinguished: (1) metaluminous I-type quartz monzonite/quartz monzodiorite (QMZD); (2) peraluminous S-type two-mica granite (TMG), which intrudes QMZD; (3) Stražanica granodiorite/quartz monzonite (GDS); and (4) isolated mafic enclaves (ME), found only in QMZD. 40K–39Ar dating a
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Shin, Seungwook, Seongjun Cho, Euijun Kim, and Jihyun Lee. "Geophysical Properties of Precambrian Igneous Rocks in the Gwanin Vanadiferous Titanomagnetite Deposit, Korea." Minerals 11, no. 10 (2021): 1031. http://dx.doi.org/10.3390/min11101031.

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Precambrian igneous rocks (851–873 Ma) occur in Pocheon City, Korea. These rocks—crystallized during magmatic differentiation—formed vanadiferous titanomagnetite (VTM) deposit. Vanadium is a crucial element in vanadium redox flow batteries that are most appropriate for large-scale energy storage systems. We investigated the VTM deposit to evaluate its size and the possible presence of a hidden orebody. We demonstrated laboratory experiments of density, susceptibility, resistivity, and chargeability of the Precambrian igneous rocks to enhance the interpretation accuracy of geophysical surveys.
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Azizi, Moussaid, Aissa Mohamed, El Azmi Mohammed, et al. "New Petro-Mineralogical Results on the Magmatic Surrounding Rocks of Cu-Ag Mineralization in Tagmout (Eastern Anti -Atlas, Morocco)." European Scientific Journal, ESJ 13, no. 36 (2017): 368. http://dx.doi.org/10.19044/esj.2017.v13n36p368.

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Tagmout deposit is located in the Eastern Anti-Atlas, about 30 km south of the city of Qalâat Mgouna. It contains Cu-Ag mineralization which is embedded in magmatic rocks that are essentially intrusive of various facies. Detailed mapping (1/1200) and petro-mineralogical observation of these facies allow us to distinguish: 1) Olivine gabronorite, it is composed mainly of pyroxenes (CPX and OPX), olivine and biotite; 2) Quartz monzogabbro, it is characterized by the presence of pyroxenes, amphiboles, plagioclases, FK and quartz; 3) Quartz monzodiorite, which is a porphyric facies. It occupies th
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Dissertations / Theses on the topic "Monzodiorite"

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Pressi, Leonardo Frederico. "Evolução magmática do plúton Piracaia (SP): parâmetros físico-químicos e evidências de mistura entre magmas monzodioríticos e sieníticos." Universidade de São Paulo, 2012. http://www.teses.usp.br/teses/disponiveis/44/44143/tde-11032013-104316/.

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O presente trabalho investiga processos de interação e mistura parcial de magmas monzodioríticos e sieníticos s.l. no Plúton Piracaia,(~ 580 Ma), que pertence à Província Granítica Itu, de caráter pós-orogênico. O Plúton Piracaia é uma intrusão alongada com cerca de 30 km2, formada por cinco unidades: Monzodioritos grossos (Mdr); Monzodioritos finos (Mdf); Monzonitos heterogêneos (Mh); Sienitos (Sie); quartzo sienitos e quartzo monzonitos (Qsie). Como base para a caracterização dos processos de interação de magmas, foram estimados os parâmetros físico-químicos dos magmas primários e híbri
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Tang, Eng Hoo Joseph. "The Petrogenesis Of The Station Creek Igneous Complex And Associated Volcanics, Northern New England Orogen." Queensland University of Technology, 2004. http://eprints.qut.edu.au/15902/.

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The Station Creek Igneous Complex (SCIC) is one of the largest Middle-Late Triassic plutonic bodies in the northern New England Orogen of Eastern Australia. The igneous complex comprises of five plutons - the Woonga Granodiorite (237 Ma), Woolooga Granodiorite (234 Ma), Rush Creek Granodiorites (231 Ma) and Gibraltar Quartz Monzodiorite and Mount Mucki Diorite (227 Ma respectively), emplaced as high-level or epizonal bodies within the Devonian-Carboniferous subduction complex that resulted from a westward subduction along the east Australian margin. Composition of the SCIC ranges from monzogab
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Laurent, Jean Christophe. "Les épisodes magmatiques filoniens basiques du massif des Ecrins-Pelvoux entre Carbonifère et Lias." Phd thesis, 1992. http://tel.archives-ouvertes.fr/tel-00509743.

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Les filons basiques du Massif des Ecrins-Pelvoux (massif cristallin externe des Alpes françaises) se rattachent à 2 principaux cortèges marqueurs de l'évolution géodynamique du domaine dauphinois entre Carbonifère et Lias : -un cortège basaltique associé à la distension du début du cycle alpin, -un cortège lamprophyrique, d'affinité subalcaline à magnésio-potassique, Carbonifère supérieur. I- Le cortège Carbonifère est formé par des lamprophyres micacès déjà connus (minettes) et également par des lamprophyres calco-alcalins à amphibole (vosgésites, quartz-monzodiorites). Ces 2 groupes présente
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Conference papers on the topic "Monzodiorite"

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Owens, Brent E., Thomas A. Johnson, and Caroline E. Polly. "GEOCHEMISTRY AND GEOCHRONOLOGY OF A MONZODIORITIC PHASE OF THE PETERSBURG BATHOLITH, EASTERN PIEDMONT PROVINCE, VIRGINIA." In Joint 69th Annual Southeastern / 55th Annual Northeastern GSA Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020se-344904.

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