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
Sun W
中科院分区:
综合性期刊1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

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早期俯冲带和弧发育的岩浆性质不同于成熟系统。伊豆-小笠原-马里亚纳(IBM)系早期以低Ti-K拉斑玄武岩和玻安岩为主。从位于IBM最古老的残余弧以西的奄美三角盆地(ASB)中发现的玄武岩喷发时间约为49 Ma。这是在以弧前玄武岩(FAB)为代表的俯冲开始(51-52 Ma)之后的300万年,处于FAB-玻安岩和典型弧岩浆作用之间的临界点。我们表明ASB玄武岩是低Ti-K、含铝尖晶石拉斑玄武岩,与大洋中脊(莫尔)、弧后盆地、岛弧或洋岛玄武岩相比有所不同。它们的上地幔源是热的、还原的、难熔的橄榄岩,这表明它们之前是熔融提取的。ASB玄武岩从斜长石-尖晶石橄榄岩相边界的压力(~0.7-2 GPa)迅速转移到地表。残留的一个polybaric-polythermal矿物保存在这个玄武岩,并没有被抹杀在持久的充电-混合-抽头-压裂制度典型的莫尔或成熟的弧。
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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