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• W2400990151 endingPage "1135" @default.
• W2400990151 startingPage "1097" @default.
• W2400990151 abstract "In continental-margin subduction zones, basalt magmas spawned in the mantle interact with the crust to produce a broad spectrum of volcanic arc associations. A distinct style of very voluminous arc volcanism develops far inland on thick crust over periods of 10–20 m.y. and involves relatively infrequent caldera-forming explosive eruptions of dominantly calc-alkaline rhyolite, dacite, and trachydacite with repose times of 104–106 yr. Volumes of individual eruptions are large (102–103 km3), and nested super-eruptions of thousands of cubic kilometers are common. Calderas are as much as 60–75 km in diameter, and surrounding individual ignimbrite outflow sheets extend outward as much as 150 km, blanketing upwards of 105 km2. Little or no basalt is extruded, whereas andesitic differentiates coeval with silicic ignimbrites range from minor to dominant in relative volume. A common feature in these flareups is essentially nonextending, thick, inland crust overlying a subducting oceanic plate with transverse tears that rolled back to a steeper dip from a previously flat configuration. Lithospheric delamination is locally possible. Large volumes of basalt that provide heat and mass for silicic magma generation in the crust form by fluid fluxing of the growing mantle wedge overlying the steepening dehydrating slab and from asthenospheric decompression. Variations in the mantle input, together with variations in crustal thickness, temperature, and composition, modulate the expression of the flareups. As a consequence of the high flux of mantle-derived magma into the thick crust, geotherms become elevated, and the brittle-ductile transition can rise to depths as shallow as 7 km. At this transition, diapirically rising magmas from a melting, assimilation, storage, and homogenization (MASH) zone are blocked and spread laterally into discoid chambers that grow until a thermomechanical threshold is attained, triggering climactic eruption and caldera collapse." @default.
• W2400990151 created "2016-06-24" @default.
• W2400990151 creator A5061438529 @default.
• W2400990151 creator A5066036713 @default.
• W2400990151 creator A5080656537 @default.
• W2400990151 creator A5090951456 @default.
• W2400990151 date "2016-05-27" @default.
• W2400990151 modified "2023-09-29" @default.
• W2400990151 title "Slab-rollback ignimbrite flareups in the southern Great Basin and other Cenozoic American arcs: A distinct style of arc volcanism" @default.
• W2400990151 cites W1489332407 @default.
• W2400990151 cites W1493429364 @default.
• W2400990151 cites W1503753826 @default.
• W2400990151 cites W1566142177 @default.
• W2400990151 cites W1581029918 @default.
• W2400990151 cites W1588903598 @default.
• W2400990151 cites W1594202803 @default.
• W2400990151 cites W1597131080 @default.
• W2400990151 cites W1826557169 @default.
• W2400990151 cites W1832101101 @default.
• W2400990151 cites W1863687942 @default.
• W2400990151 cites W1866486499 @default.
• W2400990151 cites W1896318108 @default.
• W2400990151 cites W1922607068 @default.
• W2400990151 cites W1926530879 @default.
• W2400990151 cites W1931334661 @default.
• W2400990151 cites W1950030703 @default.
• W2400990151 cites W1952657320 @default.
• W2400990151 cites W1965235751 @default.
• W2400990151 cites W1965334648 @default.
• W2400990151 cites W1971677939 @default.
• W2400990151 cites W1972635099 @default.
• W2400990151 cites W1974068301 @default.
• W2400990151 cites W1976876082 @default.
• W2400990151 cites W1977812515 @default.
• W2400990151 cites W1978100541 @default.
• W2400990151 cites W1978239619 @default.
• W2400990151 cites W1978434939 @default.
• W2400990151 cites W1978696207 @default.
• W2400990151 cites W1982118449 @default.
• W2400990151 cites W1982943020 @default.
• W2400990151 cites W1983081488 @default.
• W2400990151 cites W1983660516 @default.
• W2400990151 cites W1986407841 @default.
• W2400990151 cites W1987118288 @default.
• W2400990151 cites W1989998308 @default.
• W2400990151 cites W1991441400 @default.
• W2400990151 cites W1991797305 @default.
• W2400990151 cites W1991895753 @default.
• W2400990151 cites W1993237730 @default.
• W2400990151 cites W1994048706 @default.
• W2400990151 cites W1994337139 @default.
• W2400990151 cites W1995640473 @default.
• W2400990151 cites W1995766312 @default.
• W2400990151 cites W1999007561 @default.
• W2400990151 cites W1999125016 @default.
• W2400990151 cites W2003382314 @default.
• W2400990151 cites W2003477622 @default.
• W2400990151 cites W2004993774 @default.
• W2400990151 cites W2005846504 @default.
• W2400990151 cites W2006014937 @default.
• W2400990151 cites W2006051428 @default.
• W2400990151 cites W2008787240 @default.
• W2400990151 cites W2009477755 @default.
• W2400990151 cites W2009860990 @default.
• W2400990151 cites W2010930393 @default.
• W2400990151 cites W2011682877 @default.
• W2400990151 cites W2013303236 @default.
• W2400990151 cites W2014024368 @default.
• W2400990151 cites W2018716275 @default.
• W2400990151 cites W2023320566 @default.
• W2400990151 cites W2023391448 @default.
• W2400990151 cites W2026375484 @default.
• W2400990151 cites W2026556545 @default.
• W2400990151 cites W2026919016 @default.
• W2400990151 cites W2028397769 @default.
• W2400990151 cites W2028521621 @default.
• W2400990151 cites W2032541724 @default.
• W2400990151 cites W2036087795 @default.
• W2400990151 cites W2037611419 @default.
• W2400990151 cites W2038099198 @default.
• W2400990151 cites W2039202012 @default.
• W2400990151 cites W2039849480 @default.
• W2400990151 cites W2041487535 @default.
• W2400990151 cites W2041957817 @default.
• W2400990151 cites W2042402279 @default.
• W2400990151 cites W2048233298 @default.
• W2400990151 cites W2048341622 @default.
• W2400990151 cites W2048607926 @default.
• W2400990151 cites W2049102500 @default.
• W2400990151 cites W2049575148 @default.
• W2400990151 cites W2050553850 @default.
• W2400990151 cites W2050980355 @default.
• W2400990151 cites W2051222055 @default.
• W2400990151 cites W2051737611 @default.
• W2400990151 cites W2053071297 @default.
• W2400990151 cites W2053396208 @default.
• W2400990151 cites W2055249507 @default.
• W2400990151 cites W2056232757 @default.

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