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Caldera-forming eruptions of mushy silicic magma are among the most catastrophic natural events on Earth. In such magmas, crystals form an interlocking framework when their content reaches ...Read more ...
· The Yuleken porphyry Cu–Mo deposit is situated in the Chinese Altay-East Junggar (CAEJ) section of the Central Asian Orogenic Belt (CAOB), the world's largest Phanerozoic subduction-accretionary orogens (Carroll et al., 1990; Sengör et al., 1993; Jahn et al., 2000; Fig. 1a).The CAOB hosts several giant PCDs, e.g., Oyu Tolgoi, Samarka and Aktogai-Aiderly (Yakubchuk, 2004; Sillitoe, 2010; …Read more ...
· 1. Introduction. Granodiorites and tonalites (called here granotonalites for short) build-up more than 90% volume of cordilleran-type batholiths, which formed in response to subduction at active continental margins (Wyllie et al., 1976, Wyllie, 1977).Beside the great abundance and accessibility for study, the petrogenesis of granotonalites remains among the most debated topics in geology ...Read more ...
· The Yellowstone Plateau volcanic field is located in northwest Wyoming and southeast Idaho, USA ().It is well known for three major caldera-forming eruptions that deposited 250 to 2500 km 3 of high-silica (≤ 76 wt.% SiO 2) pyroclastic material over an immense area (Christiansen, 2001, Pierce and Morgan, 2009).The most recent caldera-forming eruption deposited the Lava Creek Tuff, 640 ± 2 ka ...Read more ...
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[1] Granitoid magmatic sheets emplaced syntectonically during growth of the Orlica‐Śnieżnik mantled gneiss dome (Central Sudetes, European Variscan belt) were examined by means of structural geology, quartz, and anisotropy of magnetic susceptibility (AMS) fabric studies. Magmatic emplacement was localized along the eastern transpressive margin of the high metamorphic core and below the low ...Read more ...
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Hazardous sequences of vulcanian explosions are thought to result from the repeated emplacement and destruction of degassed, highly crystalline magma plugs in the shallow conduit of arc volcanoes. The processes governing the timing and magnitude of these explosions are thought to be related to magma ascent rate and efficiency of degassing and crystallisation. We study a rare suite of time ...Read more ...
That is to say, the ultramafic magma hosting the Cu-Ni sulfide formed at the bottom of the staging magma chamber, while the magnetite-mineralized gabbro was in the upper part.Read more ...
That is to say, the ultramafic magma hosting the Cu-Ni sulfide formed at the bottom of the staging magma chamber, while the magnetite-mineralized gabbro was in the upper part. ... We review the ...Read more ...
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alkaline magma hosting clinopyroxenes was therefore subject to a relatively low-pressure fractionation in closed-magma chambers at different levels by means of variations in the crystallization conditions during rapid ascent of the magma, resulting from post-collision extensional tectonic regime affecting the eastern Pontides during MiddleRead more ...
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· Experimental studies demonstrate that solubility of CO 2 in silicate melts decreases strongly with decreasing pressure (e.g., Blank and Brooker, 1994).In addition, CO 2 partitions into the fluid phase as soon as magmas start to degas. Therefore, CO 2 is commonly lost through exsolution into coexisting magmatic fluids during magma ascent and eruption. The only direct approach for …Read more ...
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1 Introduction. Resurgence phenomena are common inside active calderas (e.g., de Silva et al., 2015; Kennedy et al., 2012; Lipman, 1984; Marsh, 1984; Smith & Bailey, 1968), and an ideal location for studying caldera resurgence is the Campi Flegrei caldera (CFc).Although ground movements at CF have been well documented since Roman times (Bellucci et al., 2006; Parascandola, 1947), the entity ...Read more ...
[1] Granitoid magmatic sheets emplaced syntectonically during growth of the Orlica‐Śnieżnik mantled gneiss dome (Central Sudetes, European Variscan belt) were examined by means of structural geology, quartz, and anisotropy of magnetic susceptibility (AMS) fabric studies. Magmatic emplacement was localized along the eastern transpressive margin of the high metamorphic core and below the low ...Read more ...
That is to say, the ultramafic magma hosting the Cu-Ni sulfide formed at the bottom of the staging magma chamber, while the magnetite-mineralized gabbro was in the upper part.Read more ...
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About Magmahosting.com.au coupons
| Total Offers | 1 |
| Coupon Codes | 0 |
| Deals Coupons | 3 |
| Best Discount | 80% OFF |
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