TY - JOUR

T1 - Decoding crystal fractionation in calc-alkaline magmas from the Bezymianny Volcano (Kamchatka, Russia) using mineral and bulk rock compositions

AU - Almeev, Renat R.

AU - Kimura, Jun Ichi

AU - Ariskin, Alexei A.

AU - Ozerov, Alexey Yu

N1 - Funding Information: We thank Alexander Maksimov for sharing with us his knowledge of Bezymianny Volcano, for providing some missing samples, and for stimulating discussions. We thank Vera Ponomareva for providing dating of the Kliuchevskoi cinder cones. AR thanks the Ministry of Education of Japan for financial support of the study in 2001–2003. We gratefully acknowledge Malcolm Rutherford, Maxim Portnyagin, Francois Holtz, Roman Botcharnikov and an anonymous reviewer for their insightful comments. The editorial work of Candace O'Connor and Pavel Izbekov is greatly appreciated.

PY - 2013/8/1

Y1 - 2013/8/1

N2 - We present a new dataset for whole-rock major, trace, isotopic, and phenocryst compositions indicating a genetic link between andesites of the Holocene eruptions of the Bezymianny stratovolcano (the Bezymianny stage), the andesitic to dacitic Late Pleistocene lava dome complex (the pre-Bezymianny stage), and the magnesian to high-alumina basalts of the adjacent Kliuchevskoi Volcano. We demonstrate that volcanic products from the Bezymianny stage of volcano evolution are most likely the products of magma mixing between silicic products of the earliest stages of magma fractionation and the less evolved basaltic andesite parental melts periodically injected into the magma reservoir. In contrast, the intermediate and silicic magmas of the pre-Bezymianny stage together with basalts from Kliuchevskoi much more closely resemble the liquid line of descent and may represent a unique prolonged and continuous calc-alkaline trend of magma evolution from high-magnesian basalt to dacite. As a result of the geothermobarometry, we recognize variable conditions of magma fractionation and magma storage beneath Bezymianny for different magma types during its evolution since the Late Pleistocene: (1) 1100-1150°C, 500-640MPa, 1-2.5wt.% H2O for parental basaltic andesite; (2) 1130-1050°C, 700-600MPa, 2.5-5wt.% H2O for two-pyroxene andesites; (3) 1040-990°C, 560-470MPa, 5-6.5wt.% H2O for orthopyroxene-bearing andesites; (4) 950-1000°C, 450-150MPa, 3.5-5.5wt.% H2O for hornblende-bearing andesites; and (5) 950-900°C, 410-250MPa, 6-7wt.% H2O for dacites. Repeated basalt injections and magma fractionation combined with internal mixing in the magma chamber are the main processes responsible for both the complex petrography and the geochemical trends observed in the lavas of Bezymianny Volcano.

AB - We present a new dataset for whole-rock major, trace, isotopic, and phenocryst compositions indicating a genetic link between andesites of the Holocene eruptions of the Bezymianny stratovolcano (the Bezymianny stage), the andesitic to dacitic Late Pleistocene lava dome complex (the pre-Bezymianny stage), and the magnesian to high-alumina basalts of the adjacent Kliuchevskoi Volcano. We demonstrate that volcanic products from the Bezymianny stage of volcano evolution are most likely the products of magma mixing between silicic products of the earliest stages of magma fractionation and the less evolved basaltic andesite parental melts periodically injected into the magma reservoir. In contrast, the intermediate and silicic magmas of the pre-Bezymianny stage together with basalts from Kliuchevskoi much more closely resemble the liquid line of descent and may represent a unique prolonged and continuous calc-alkaline trend of magma evolution from high-magnesian basalt to dacite. As a result of the geothermobarometry, we recognize variable conditions of magma fractionation and magma storage beneath Bezymianny for different magma types during its evolution since the Late Pleistocene: (1) 1100-1150°C, 500-640MPa, 1-2.5wt.% H2O for parental basaltic andesite; (2) 1130-1050°C, 700-600MPa, 2.5-5wt.% H2O for two-pyroxene andesites; (3) 1040-990°C, 560-470MPa, 5-6.5wt.% H2O for orthopyroxene-bearing andesites; (4) 950-1000°C, 450-150MPa, 3.5-5.5wt.% H2O for hornblende-bearing andesites; and (5) 950-900°C, 410-250MPa, 6-7wt.% H2O for dacites. Repeated basalt injections and magma fractionation combined with internal mixing in the magma chamber are the main processes responsible for both the complex petrography and the geochemical trends observed in the lavas of Bezymianny Volcano.

KW - Bezymianny Volcano

KW - Calc-alkaline trend of magma differentiation

KW - Fractional crystallization

KW - Link between HMBs, HABs, andesites and dacites

KW - Magma mixing

UR - http://www.scopus.com/inward/record.url?scp=84885186461&partnerID=8YFLogxK

U2 - http://repo.kscnet.ru/2546/1/2013_Almeev-Bezy.pdf

DO - http://repo.kscnet.ru/2546/1/2013_Almeev-Bezy.pdf

M3 - Article

AN - SCOPUS:84885186461

VL - 263

SP - 141

EP - 171

JO - Journal of Volcanology and Geothermal Research

JF - Journal of Volcanology and Geothermal Research

SN - 0377-0273

ER -