Basalt derived from highly refractory mantle sources during early Izu-Bonin-Mariana arc development.
Basalt derived from highly refractory mantle sources during early Izu-Bonin-Mariana arc development.
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玄武岩源自早期伊豆-小笠南-马里亚纳岛弧发育过程中的高难熔地幔源
DOI:
10.1038/s41467-021-21980-0
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发表时间:
2021-03-19
影响因子:
16.6
通讯作者:
Sun W
中科院分区:
文献类型:
--
作者:
Li H;Arculus RJ;Ishizuka O;Hickey-Vargas R;Yogodzinski GM;McCarthy A;Kusano Y;Brandl PA;Savov IP;Tepley FJ 3rd;Sun W
The magmatic character of early subduction zone and arc development is unlike mature systems. Low-Ti-K tholeiitic basalts and boninites dominate the early Izu-Bonin-Mariana (IBM) system. Basalts recovered from the Amami Sankaku Basin (ASB), underlying and located west of the IBM’s oldest remnant arc, erupted at ~49 Ma. This was 3 million years after subduction inception (51-52 Ma) represented by forearc basalt (FAB), at the tipping point between FAB-boninite and typical arc magmatism. We show ASB basalts are low-Ti-K, aluminous spinel-bearing tholeiites, distinct compared to mid-ocean ridge (MOR), backarc basin, island arc or ocean island basalts. Their upper mantle source was hot, reduced, refractory peridotite, indicating prior melt extraction. ASB basalts transferred rapidly from pressures (~0.7-2 GPa) at the plagioclase-spinel peridotite facies boundary to the surface. Vestiges of a polybaric-polythermal mineralogy are preserved in this basalt, and were not obliterated during persistent recharge-mix-tap-fractionate regimes typical of MOR or mature arcs.
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影响因子:
3.9
作者:
ARCULUS, RJ;WILLS, KJA
通讯作者:
WILLS, KJA
影响因子:
3.5
作者:
Herzberg, C.;Asimow, P. D.
通讯作者:
Asimow, P. D.
影响因子:
3.5
作者:
Gale, Allison;Dalton, Colleen A.;Schilling, Jean-Guy
通讯作者:
Schilling, Jean-Guy
影响因子:
5.3
作者:
HOFMANN, AW;JOCHUM, KP;WHITE, WM
通讯作者:
WHITE, WM
影响因子:
5.3
作者:
Gurnis, Michael;Van Avendonk, Harm;Carrington, Luke
通讯作者:
Carrington, Luke