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首页> 外文期刊>Journal of South American earth sciences >Tectonic implications of the Jurassic magmatism and the metamorphic record at the southern Colombian Andes
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Tectonic implications of the Jurassic magmatism and the metamorphic record at the southern Colombian Andes

机译:侏罗纪魔法学的构造影响与南部哥伦比亚南部的变质记录

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摘要

The Jurassic magmatism and metamorphism of Colombia result from the convergent relation between the Farall acute accent on plate and the northwestern continental margin of South America. However, the geodynamic process that generated both magmatism and metamorphism is still unclear. Field relations, U-Pb geochronology and trace elements in zircons, whole-rock geochemistry, and mineral chemistry from a series of plutonic and metamorphic rocks found in Narin tilde o and Putumayo regions (southern Colombia) were used to constrain their composition, age, relation, and tectonic setting, as well correlate them with the Jurassic continental magmatic arc of Colombia. The plutonic rocks vary compositionally from diorite to granite. Whole-rock geochemical analyses show relative enrichment of Large Ion Lithophile Elements (LILE) and Light Rare Earth Elements (LREE) compared with High Field Strength Elements (HFSE) and Heavy Rare Earth Elements (LREE), and negative Nb and Ti anomalies, which reveal that the samples were formed in a volcanic arc setting. U-Pb zircon geochronology indicates that the granitoids crystallized during the Late Jurassic (ca. 163-153 Ma). On the other hand, the metamorphic rocks are hornblende-biotite schists that yield a U-Pb age of 160.8 +/- 0.8 Ma, considered the crystallization age of the protolith. Pressure-temperature (P-T) calculations indicate that the schists underwent metamorphism at similar to 700 degrees C and 0.45 GPa.The results obtained enable us to correlate the granitoids with the Jurassic magmatic arc of the Colombian Andes. Furthermore, the hornblende-biotite schist is probably contemporaneous with amphibolites and metapelites reported farther north in the Central Cordillera (Cajamarca Complex), which indicates that they could be part of a regional scale metamorphic belt either exposing different structural levels or recording metamorphic conditions from different positions in an arc-related setting.
机译:侏罗纪魔法师和哥伦比亚的变质作用是由盘子和南美洲的西北大陆边缘的Farall急性口音之间的收敛关系。然而,产生岩浆学和变质性的地球动力学过程仍然不清楚。从Narin Tilde O和Putumayo地区(南部哥伦比亚南部)发现的锆石,全岩地球化学和矿物化学中的U-PB地球化学和矿物化学中的微量元素用于约束其组合,年龄,关系和构造环境以及与侏罗纪的巨大的哥伦比亚大陆岩弧相关联。浮雕岩石从Diorite到花岗岩改变。全岩地球化学分析表明,与高场强元素(HFSE)和重质稀土元素(LREE)和负NB和Ti异常相比,相对富集的大离子绞合元件(含量)和轻质稀土元素(LREE)的相对富集。揭示样品在火山电弧环境中形成。 U-PB锆石地理学表明,在侏罗纪晚期(约163-153MA)中结晶的花岗岩。另一方面,变质岩石是Hornblende-Biotite Schist,其产生U-PB Age的160.8 +/- 0.8 mA,认为是促果实的结晶年龄。压力 - 温度(P-T)计算表明,SCIST接受了类似于700℃和0.45GPa的变质。结果使我们能够将花岗岩与哥伦比亚山脉的侏罗纪岩弧弧相关联。此外,Hornblende-Biotite Schist可能是倒置的倒置和北北部的朝北(Cajamarca Complex)的北北方,这表明它们可以成为区域尺度变质带的一部分,可以暴露不同的结构水平或从不同的记录变质条件在电弧相关设置中的位置。

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