Mantle temperature control on composition of arc magmas along the Central Kamchatka Depression.

Portnyagin, Maxim and Manea, Vlad C. (2008) Mantle temperature control on composition of arc magmas along the Central Kamchatka Depression. Geology, 36 . pp. 519-522. DOI 10.1130/G24636A.1.

[img] Text
104_Portnyagin_2008_MantleTemperatureControlOnComposition_Artzeit_pubid9335.pdf - Reprinted Version
Restricted to Registered users only

Download (1235Kb) | Contact

Supplementary data:


Abundant volcanism in the Central Kamchatka Depression (CKD) adjacent to the Kamchatka–Aleutian Arc junction occurs where the Pacific slab edge is subducting beneath Kamchatka. Here we summarize published data on CKD rocks and demonstrate a systematic south-to-north change of their compositions from moderately fractionated basalt-andesite tholeiitic series to highly fractionated basalt-rhyolite calc-alkaline series including high-magnesian andesites near the slab edge. Localized slab melting at the slab edge cannot explain these regional geochemical variations. Instead, we propose that the thermal state of the mantle wedge can be the key factor governing the composition of CKD magmas. We integrate the results from petrology and numeric modeling to demonstrate the northward decrease of the mantle wedge temperatures beneath CKD volcanoes, which correlates with decreasing slab dip, length of mantle columns, and magma flux. We envision two petrogenetic models, which relate the composition of erupted magmas to the subduction parameters beneath the CKD. The first model suggests that mantle temperature governs melt-peridotite equilibria and favors generation of andesitic primary melts in cold mantle regions above the shallowly subducting Pacific slab edge. Alternatively, mantle temperature may control magmatic productivity along the CKD, which decreases sharply toward the slab edge and thus allows more extensive magma fractionation deeper in the crust and mixing of highly evolved and mantle-derived magmas to generate Si-rich “primitive” magmas. These results point to a possible casual link between deep mantle and shallow crustal magmatic processes. Similar effects of mantle temperature on the composition and productivity of arc magmatism are expected elsewhere, particularly in volcanic regions associated with significant slab dip variation along the arc.

Document Type: Article
Keywords: Kamchatka, island arc, subduction, calc-alkaline, tholeiite, high-magnesian andesite, mantle wedge, mixing, numeric modeling
Research affiliation: OceanRep > SFB 574 > C2
OceanRep > SFB 574
OceanRep > GEOMAR > FB4 Dynamics of the Ocean Floor > FB4-MUHS
Refereed: Yes
Open Access Journal?: No
DOI etc.: 10.1130/G24636A.1
ISSN: 0091-7613
Projects: SFB574
Contribution Number:
SFB 574151
Date Deposited: 03 Dec 2008 16:52
Last Modified: 24 Oct 2019 12:12

Actions (login required)

View Item View Item

Document Downloads

More statistics for this item...