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Mesoproterozoic Oaxaquia-type basement in peri-Gondwanan terranes of Mexico, the Appalachians, and Europe: T DM age constraints on extent and significance

机译:墨西哥,阿巴拉契亚和欧洲贡多瓦南近地中元古代的Oaxaquia型基底:T DM 年龄限制的程度和意义

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The basement of most peri-Gondwanan terranes in Mexico, the Appalachians, the Caledonides, and the Variscides is buried beneath younger Ediacaran arc, Palaeozoic passive margin, and/or Mesozoic-Cenozoic platformal carbonates. However, it is exposed in the Oaxaquia terrane of Mexico (Oaxacan, Novillo, Huiznopala, and Guichicovi complexes), where it is characterized by ca. 1.0-1.3 billion year protolith ages and igneous rocks with depleted mantle model ages (T DM) of 1.35-1.77 billion years. The T DM ages represent a bulk average composition of the source and can be used as a tracer; these T DM ages overlap with those in ca. 546 Ma arc clasts from the 65.5 Ma Chicxulub bolide breccia, suggesting that the northern Maya block is also underlain by Oaxaquia-type basement. Similar T DM ages occur in Ediacaran arc rocks in Suwannee (Florida), NW Avalonia, Ganderia, Iberia, Armorica, and Bohemia, and in lower Palaeozoic plutons cutting adjacent Palaeozoic passive margin rocks (Acatlán Complex, Gander Group), suggesting that Oaxaquia-type basement underlies these regions. These T DM ages are intermediate between those of SE Avalonia/Carolinia (0.75-1.1 billion years) and the ca. 2.0 Ga basement typical of NW Africa and the Channel Islands of the United Kingdom. The lateral extent of this Oaxaquia-type basement suggests that it formed a Precambrian rim around the periphery of northern Gondwana (Amazonia and NW Africa). The Oaxaquia-type basement beneath Ganderia and northwestern Avalonia suggests that these terranes were derived from the Oaxaquia margin of Amazonia. The polarity of the T DM ages in Avalonia (younger to the SE) suggests that, rather than being transferred orthogonally across Iapetus, these peri-Gondwanan terranes rotated clockwise through 90° before accretion to Laurentia.View full textDownload full textKeywordsOaxaquia, peri-Gondwanan terranes, T DM ages, palaeogeographic reconstructionsRelated var addthis_config = { ui_cobrand: "Taylor & Francis Online", services_compact: "citeulike,netvibes,twitter,technorati,delicious,linkedin,facebook,stumbleupon,digg,google,more", pubid: "ra-4dff56cd6bb1830b" }; Add to shortlist Link Permalink http://dx.doi.org/10.1080/00206814.2010.543783
机译:墨西哥大多数冈多瓦南地层,阿巴拉契亚山脉,喀里多尼德群岛和瓦里西德群岛的地下被埋在较年轻的埃迪卡拉纪弧线,古生代被动边缘和/或中生代-新生代平台性碳酸盐岩之下。但是,它暴露于墨西哥的Oaxaquia地貌(Oaxacan,Novillo,Huiznopala和Guichicovi配合物),其特征为大约。 1.0-13亿年的原生石年龄和火成岩的地幔模型年龄(T DM )为1.35-17.7亿年。 T DM 年龄代表了来源的总体平均构成,可以用作示踪剂。这些T DM 年龄与大约。 546 Ma弧形碎片来自65.5 Ma Chicxulub泥石流角砾岩,表明北部玛雅块体也位于Oaxaquia型地下室的下面。相似的T DM 年龄发生在Suwannee(佛罗里达),西北阿瓦龙尼亚,Ganderia,Iberia,Armorica和Bohemia的Ediacaran弧岩中,以及在下古生界岩体中切割相邻的古生界被动边缘岩石(AcatlÃnComplex ,Gander Group),表明Oaxaquia型地下室是这些区域的基础。这些T DM 年龄介于SE Avalonia / Carolinia(0.75-11亿年)和大约。典型的西北非洲和联合王国的海峡群岛2.0 Ga地下室。该Oaxaquia型地下室的横向范围表明,它在冈瓦纳北部(亚马逊和西北非洲)的外围形成了前寒武纪边缘。甘德里亚(Ganderia)和西北阿瓦隆(Avalonia)西北部的瓦哈基亚(Oaxaquia)型基底表明,这些地层来自亚马逊河的瓦哈基亚边缘。 Avalonia(小于SE)的T DM 年龄的极性表明,这些Gondwanan周围的土层不是垂直地跨过Iapetus转移,而是顺时针旋转90°,然后才增加到Laurentia。全文下载关键字关键词瓦哈基亚(Oaxaquia),贡多瓦南山脉(Ter-Gondwanan terranes),T DM年龄,古地理重建,more“,pubid:” ra-4dff56cd6bb1830b“};添加到候选列表链接永久链接http://dx.doi.org/10.1080/00206814.2010.543783

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