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首页> 外文期刊>Gondwana research: international geoscience journal >Constraints on the subduction erosion/extrusion cycle in the Paleozoic Acatlán Complex of southern Mexico: Geochemistry and geochronology of the type Piaxtla Suite
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Constraints on the subduction erosion/extrusion cycle in the Paleozoic Acatlán Complex of southern Mexico: Geochemistry and geochronology of the type Piaxtla Suite

机译:墨西哥南部古生代阿卡特兰复合体俯冲侵蚀/挤压循环的约束:Piaxtla Suite类型的地球化学和地球年代学

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The type high-pressure (HP) Piaxtla Suite in the Acatlán Complex of southern Mexico consists of retrogressed eclogite (amphibolite), megacrystic granitoids and high-grade meta-sedimentary rocks. Exhumation of these HP rocks has recently been interpreted as the result of extrusion into the upper plate, rather than by return flow up the subduction zone. Geochemical analyses of the retrograde eclogites indicate that they have a rift tholeiitic-transitional alkalic composition. These are closely associated with a megacrystic meta-granitoid that has yielded an intrusive age of 452±6Ma (concordant U-Pb zircon analyses) with inherited zircon populations at ca. 800-950Ma and 1000-1200Ma derived from the underlying basement, probably the Oaxacan Complex which borders the Acatlán Complex to the east. The bimodal nature of these igneous rocks and their spatial and temporal close association with continentally-derived sedimentary rocks is similar to most HP rocks in the Acatlán Complex derived from a rifted passive margin. The youngest detrital zircon population in a meta-psammite sample yielded a U-Pb age of 365±15Ma with older analyses distributed along a chord with an upper intercept of 1287±29Ma. The ca. 365Ma age provides a maximum age for the time of deposition of this sample. ~(40)Ar/ ~(39)Ar ages from the retrogressed eclogites provided hornblende plateau ages of 342±2Ma and 344±2Ma, whereas muscovite from the granitoid and meta-psammite yielded 334±2Ma plateau ages. These data constrain the subduction erosion-extrusion cycle to &le35Ma during which the rocks were taken to a depth of ca. 40km at a rate of 2.7km/Ma and back to the surface at 2.4km/Ma. Such exhumation rates are slower than those in continent-continent collision zones, but similar to those in the Iberia-Czech Variscan belt where tectonic interpretation also suggests extrusion into the upper plate.
机译:墨西哥南部阿卡特兰综合体中的高压(HP)Piaxtla套件类型包括倒退的榴辉岩(闪石),大晶花岗岩和高档的准沉积岩。这些HP岩石的发掘最近被解释为挤压到上板的结果,而不是通过沿俯冲带的回流。对逆向榴辉岩的地球化学分析表明,它们具有不规则的过渡-过渡性碱性成分。这些与大晶间类nit质类密切相关,后者的侵入年龄为452±6Ma(一致的U-Pb锆石分析),遗传锆石的数量大约为。 800-950Ma和1000-1200Ma来自底层地下室,可能是与阿卡特兰山脉东侧接壤的Oaxacan建筑群。这些火成岩的双峰性质以及它们与大陆衍生的沉积岩的时空紧密联系,类似于阿卡特兰山脉复杂区中从裂谷被动缘衍生而来的大多数高压岩石。偏硅灰石样品中最年轻的碎屑锆石种群产生的U-Pb年龄为365±15Ma,沿该弦分布的较旧分析的最高截距为1287±29Ma。该ca。 365Ma年龄为该样品的沉积提供了最大年龄。渐进榴辉岩的〜(40)Ar /〜(39)Ar年龄提供了角闪石高原年龄,分别为342±2Ma和344±2Ma,而花岗岩和变质白云母的白云母产生了334±2Ma的高原年龄。这些数据将俯冲冲蚀-挤压循环限制在&le35Ma,在此期间岩石被带到了大约ca的深度。以2.7km / Ma的速度行驶40公里,然后以2.4km / Ma的速度返回地面。这样的掘尸速度比大陆-大陆碰撞带要慢,但是与伊比利亚-捷克瓦里斯卡纳带的构造相似,在构造解释上也暗示了挤压到上板块中。

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