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Gotowe bibliografie tematyczne / Subvolcanic Bodies

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Gotowa bibliografia na temat „Subvolcanic Bodies”

Autor: Grafiati

Data publikacji: 3 czerwca 2025

Data aktualizacji: 31 lipca 2025

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Artykuły w czasopismach na temat "Subvolcanic Bodies"

1

Armienti, Pietro, Claudia Corazzato, Gianluca Groppelli, Emanuele Natoli, and Giorgio Pasquarè. "Geological and Petrographical study of Montecampione Triassic subvolcanic bodies (Southern Alps, Italy): preliminary geodynamic results." Boll. Soc. Geol. It. Volume speciale n. 2 (2003), no. 2 (2003) (2003): 67–78. https://doi.org/10.5281/zenodo.836827.

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The research began with a geological and structural survey of the Triassic subvolcanic bodies cropping out in the area of Montecampione (Val Camonica-BS, Italy). This study allowed the determination of the main phases of intrusion of these bodies, and new and significant sampling of the magmatic rocks in order to reconstruct the geodynamic framework based on high quality geochemical analyses. These intrusive bodies, belonging to the «Montecampione group», show a minimum volume of about 1 km3 and could represent a shallow (about 1000 m) magmatic reservoir producing a volcanic area, since we rec

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2

Ostapenko, Nikolay, and Olga Neroda. "On the genesis of the gold-silver deposit Kupol (North-East of Russia)." Domestic geology, no. 4-5 (October 27, 2020): 39–47. http://dx.doi.org/10.47765/0869-7175-2020-10022.

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A new version of genesis of the epithermal gold-silver deposit Kupol (Chukotka), its mineral composition of ores and conditions of ore-localization based on the analysis of published geological materials on the geological structure had purposed in this article. The active thermal ore-forming role of completing the volcanic cycle of the multiphase subvolcanic complex’ the proximal bodies of the Upper Cretaceous rhyolites had been proved. The main factors of this deposit’ formation and the conditions that favored the appearance of large ore bodies and rich ores were considered. The magma chamber

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Kokovkin, Aleksandr. "On the genesis of the gold-silver deposit Kupol (North-East of Russia)." Domestic geology, no. 4-5 (October 27, 2020): 48–63. http://dx.doi.org/10.47765/0869-7175-2020-10023.

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A new version of genesis of the epithermal gold-silver deposit Kupol (Chukotka), its mineral composition of ores and conditions of ore-localization based on the analysis of published geological materials on the geological structure had purposed in this article. The active thermal ore-forming role of completing the volcanic cycle of the multiphase subvolcanic complex’ the proximal bodies of the Upper Cretaceous rhyolites had been proved. The main factors of this deposit’ formation and the conditions that favored the appearance of large ore bodies and rich ores were considered. The magma chamber

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4

Kucharič, Ľudovít, Vladimír Bezák, Dušan Majcin, and Ján Vozár. "Carbonate complexes underlying Flysch belt and subsurface Neogene volcanic in the NE part of Slovakia – a potential for geothermal energy and raw materials." Contributions to Geophysics and Geodesy 42, no. 4 (2012): 283–94. http://dx.doi.org/10.2478/v10126-012-0013-8.

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Abstract A positive gravity anomaly was observed in the Flysch belt realm. Based on this fact and available geological knowledge we suppose that the source of gravity anomaly might be carbonate rocks lying perhaps in the footwall of Flysch sediments. The carbonates belong perhaps to the Penninic crust cover (a part of Klippen belt), or to lower structural stage of the Flysch belt. Besides this it is interpreted more volume of Neogene subvolcanic bodies in the frame of the Flysch belt based on the results of the newest magnetic measurements in the NE part of Slovakia (Kucharič et. al., in press

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5

Pasenko, A. M., I. V. Fedyukin, and V. E. Pavlov. "TWO PULSES OF MAGMATIC ACTIVITY DURING THE EARLY RIPHEAN KUONAMKA IGNEOUS PROVINCE FORMATION: PALEOMAGNETIC SUBSTANTIATION OF THE HYPOTHESIS." Geodynamics & Tectonophysics 15, no. 2 (2024): 0748. http://dx.doi.org/10.5800/gt-2024-15-2-0748.

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By the beginning of the 20th century, at least ten different generations of intrusive mafic bodies 1800–900 Ma were distinguished on the territory of the Anabar massif. The first modern age estimates, however, indicate the formation of the bulk of these bodies in a relatively short period of time ~1480–1500 Ma. Based on geochronological and paleomagnetic data, intrusive bodies with this age were combined into the Kuonamka large igneous province (LIP). However, a complex of paleomagnetic studies indicated the probable existence of at least two pulses of magmatic activity during the formation of

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Parada, Sergei G. "Petrochemical Features and Formation Affiliation of Igneous Rocks of the Kondakov Uplift (Eastern Donbass)." UNIVERSITY NEWS. NORTH-CAUCASIAN REGION. NATURAL SCIENCES SERIES, no. 4-2 (December 23, 2024): 59–66. https://doi.org/10.18522/1026-2237-2024-4-2-59-66.

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The ore specialization of mineral manifestations associated with igneous rocks depends on the formation affiliation of the latter, since specific igneous formations are characterized by a certain type of metallogeny. Therefore, the identification of the formation affiliation of igneous rocks of the Kondakov tectonic uplift (KTU) makes it possible to assess metallogenic specialization and make a forecast of mineralization. For this purpose, geological mapping data and the results of prospecting works, 145 chemical analyses of igneous rocks were used. The identification of magmatic bodies was ca

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7

Tau, M. M., R. Bolhar, A. H. Wilson, and C. R. Anhaeusser. "The petrogenesis and emplacement mechanism of layered ultramafic-mafic complexes of the Barberton Greenstone Belt: Insights from the Stolzburg Complex, South Africa." South African Journal of Geology 125, no. 2 (2022): 133–66. http://dx.doi.org/10.25131/sajg.125.0013.

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Abstract Ultramaﬁc-maﬁc layered complexes are important but not-well studied components of Archaean granitoid-greenstone terranes. In the vicinity of the Barberton Greenstone Belt (BGB), at least 27 such complexes are intimately associated with the supracrustal succession. The petrogenesis of one of these layered bodies, the Stolzburg Complex (SC), is explored, together with its relationship to the surrounding Barberton volcanic succession. Previous models for the origin of Barberton layered complexes proposed a variety of mechanisms, such as single chamber subvolcanic sills, ponded lavas, and

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Platten, I. M., and M. S. Money. "Formation of late Caledonian subvolcanic breccia pipes at Cruachan Cruinn, Grampian Highlands, Scotland." Transactions of the Royal Society of Edinburgh: Earth Sciences 78, no. 2 (1987): 85–103. http://dx.doi.org/10.1017/s0263593300011007.

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ABSTRACTPipe-shaped breccia bodies associated with diorite intrusions are composed mainly of angular clasts of local schists with a few transported clasts of quartzite. Plate shaped fragments are commonly oriented to define planar fabrics in the breccias. These features indicate the operation of gas fluidisation within the pipes and both entrainment and expanded bed conditions are inferred. The fabrics result from the collapse of the fluidised suspensions as the gas flow declined. Dilational fracture patterns in the country rock comparable with the stress release patterns found around mine sha

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9

STEPANOV, VITALY, and ANTON MELNIKOV. "THE SNEZHINKA GOLD ORE DEPOSIT IN THE URKINSKY ORE-PLACER CLUSTER OF THE AMUR PROVINCE." Domestic geology, no. 3 (July 14, 2022): 22–31. http://dx.doi.org/10.47765/0869-7175-2022-10013.

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The article is devoted to characteristics of the Snezhninka gold deposit in the Urkinsky ore-placer cluster of the Amur gold-bearing province. It presents information on the structural-geological position and geological features of the deposit, regularities of distribution of the ore bodies, and the ore composition. The ore bodies are represented by zones of quartz-veinlet silicification and, more rarely, by carbonate-quartz veins among beresitized granites. The ore minerals, comprising no more than a few percent of the ore volume, are represented by pyrite, chalcopyrite, arsenopyrite, galena,

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10

Pécskay, Zoltán, Alexandra Harkovska, and Alexander Hadjiev. "K-Ar dating of Mesta volcanics (SW Bulgaria)." Geologica Balcanica 30, no. 1-2 (2000): 3–11. http://dx.doi.org/10.52321/geolbalc.30.1-2.3.

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The Mesta volcanic massif (SW Bulgaria) belongs to the Macedonian-Rhodope-North Aegean Magmatic Zone. It crops out along the middle course of Mesta River and covers about 200 km2 of the homonymous graben. The bаsеmеnt of Mesta graben and the neighbouring elevated blocks of Pirin and Western Rhodope mountains are composed of high-grade metamorphics, hosting granitoidic plutons of diverse ages, including the Paleogene Central Pirin and Teshevo plutons. Apart from the volcanic bodies, the graben-fill consists of complexly interfingered Paleogene stratified continental terrigenous sedimentary rock

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