Lithospheric weakspots, not hotspots: New England-Quebec and Shenandoah anorogenic magmatism in the context of global plate tectonics, intraplate stress and LIPs

IF 10.8 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Peter R. Vogt , Gillian R. Foulger
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引用次数: 0

Abstract

We explore the origins of anorogenic post-breakup magmatism in two areas of the mid-Atlantic Appalachians: the New England-Quebec Province (ca. 130–120 Ma) and the Shenandoah Province (ca. 49–47 Ma). Radiometric rock ages and other data do not support claims that this magmatism occurred when these sites were located above postulated Great Meteor and Bermuda mantle hotspots/plumes. We propose instead that the sites are persistent lithospheric ‘weakspots’ favorable for magma ascent during relatively short intervals of a few Myr when global-scale plate motion reorganizes every 20–30 Myr. Magma ascends into the crust when compressive intra-plate stress is relaxed. Weakspots in the plate, not fixed mantle hotspots, can explain why anorogenic magmatism occurred at the same two sites also much earlier (by ca. 50 Myr in the New England-Quebec province and ca. 100 Myr in the Shenandoah Province), and why the Bermuda volcanoes formed not later, but coevally with the Shenandoah Province, 1400 km along the postulated hotspot trace. The plume hypothesis also fails to explain why the New England-Quebec magmas were emplaced at the same time as anomalously productive magmatism along the northern mid-Atlantic Ridge and coincident with the breakup of Iberia from the Grand Banks, sites almost 2000 km distant from the New England-Quebec Province. Moreover, New England-Quebec radiometric age distributions suggest that distant magmatic events and continental breakup affecting other plates were global plate reorganization events that may be ‘recorded’ by volcanism at weakspots. Shenandoah-Bermuda magmatism happened during the Pacific plate motion change recorded by the Hawaii-Emperor Bend. The ca. 720 Ma Robertson River Igneous Suite of anorogenic plutons in Virginia, USA, may be an old analog of the Shenandoah Province exploiting the same lithospheric weakspot. The New England-Quebec magmatic period 130–120 Ma is also the time over which the geomagnetic reversal frequency slowed, reaching zero at the onset of the Cretaceous normal superchron (C34n) at ca. 120 Ma. This event was recorded at the mid-Atlantic Ridge axis as the J-Anomaly Ridge and a large increase in spreading half-rate from 1 to 2.5 cm/a. Thus, geomagnetic reversal frequency may also be related to plate tectonics.
岩石圈弱点而非热点:从全球板块构造、板块内部应力和 LIPs 的角度看新英格兰-魁北克和谢南多纳同源岩浆活动
我们在大西洋中部阿巴拉契亚山脉的两个地区:新英格兰-魁北克省(约 130-120 Ma)和谢南多省(约 49-47 Ma)探索了断裂后原生岩浆活动的起源。放射性岩石年龄和其他数据并不支持这样的说法,即岩浆活动发生时,这些地点位于推测的大流星和百慕大地幔热点/羽流之上。相反,我们认为这些地点是岩石圈的持续性 "薄弱点",在全球尺度板块运动每 20-30 Myr 进行重组时,在相对较短的几 Myr 间隔内有利于岩浆上升。当板块内压应力松弛时,岩浆就会上升到地壳中。板块中的薄弱点,而不是固定的地幔热点,可以解释为什么在同样的两个地点也会更早地出现源生岩浆活动(在新英格兰-魁北克省约为 50 Myr,在谢南多尔省约为 100 Myr),以及为什么百慕大火山不是后来形成的,而是与谢南多尔省同时形成的,沿着假定的热点轨迹 1400 公里。羽流假说也无法解释为什么新英格兰-魁北克岩浆与大西洋中脊北部的异常高产岩浆同时喷出,并且与伊比利亚从大浅滩(距离新英格兰-魁北克省近 2000 公里的地点)分裂的时间相吻合。此外,新英格兰-魁北克辐射年龄分布表明,遥远的岩浆事件和影响其他板块的大陆断裂是全球板块重组事件,可能被薄弱点的火山活动 "记录 "下来。神户-百慕大岩浆活动发生在夏威夷-皇帝弯记录的太平洋板块运动变化期间。约 720 Ma 的罗伯逊河岩浆岩群美国弗吉尼亚州的罗伯逊河岩浆岩组(Robertson River Igneous Suite of anorogenic plutons)约 720 Ma,可能是利用同一岩石圈薄弱点的神南多省的古老类似物。新英格兰-魁北克岩浆期 130-120 Ma 也是地磁反转频率减慢的时期,在大约 120 Ma 的白垩纪正常超同步(C34n)开始时达到零。120 Ma。这一事件在大西洋中脊轴线上被记录为J-异常脊,扩张半速率从1 cm/a大幅增加到2.5 cm/a。因此,地磁反转频率也可能与板块构造有关。
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来源期刊
Earth-Science Reviews
Earth-Science Reviews 地学-地球科学综合
CiteScore
21.70
自引率
5.80%
发文量
294
审稿时长
15.1 weeks
期刊介绍: Covering a much wider field than the usual specialist journals, Earth Science Reviews publishes review articles dealing with all aspects of Earth Sciences, and is an important vehicle for allowing readers to see their particular interest related to the Earth Sciences as a whole.
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