Pervasive crustal reworking along the proto-Andean margin of northern Peru and southern Ecuador: Insights from U-Pb, geochemical, and isotopic analyses of zircon

IF 1.7 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY
Sandoval Espinel Leidy Carolina , Witt Cesar , Zattin Massimiliano , Poujol Marc , Bruguier Olivier , Chiaradia Massimo , Bermudez Mauricio
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Abstract

Continental growth at convergent margins is the result of complex interactions between mantle additions and crustal reworking. This study examines the pre-Andean tectono-magmatic evolution of the central-northern Andean margin (∼1°S to ∼6°S) using U-Pb geochronology, trace element analysis, and εHf(t) and δ18O isotopic data from zircons embedded within detrital and bedrock samples. U-Pb dating revealed two primary clusters: a Late Neoproterozoic population (640–550 Ma) associated with the Brasiliano/Pan-African orogeny and a Permian–Triassic population (280–200 Ma) associated with the Gondwanides orogeny. There were also two minor clusters at ∼960 Ma and ∼345 Ma. Zircon grains dating between 1000 and 200 Ma crystallized during repeated episodes of crustal reworking, characterized by highly evolved εHf(t) signatures (−10 to −30) at 640–510 Ma that are indicative of ancient Amazonian cratonic sources, with no evidence of Pampean or Famatinian contributions. The results also show a marked increase in juvenile input during the Carboniferous (380–310 Ma), followed by predominantly continental input as indicated by persistently high δ18O values up to 220 Ma. Although the U-Pb age spectra of these samples are similar to that of the central Andes, isotopic and geochemical data reveal that the central-northern Andean margin evolved within a tectonic context that is more closely aligned with central-eastern Gondwana (i.e., central Africa and eastern South America) rather than typical Andean settings.
沿秘鲁北部和厄瓜多尔南部原安第斯山脉边缘的普遍地壳改造:来自锆石U-Pb、地球化学和同位素分析的见解
收敛边缘的大陆生长是地幔补充和地壳改造之间复杂相互作用的结果。本研究利用U-Pb年代学、微量元素分析以及碎屑和基岩样品中嵌入的锆石的εHf(t)和δ18O同位素数据,研究了安第斯中北部边缘(~ 1°S至~ 6°S)的前安第斯构造-岩浆演化。U-Pb测年揭示了两个主要群体:与Brasiliano/泛非造山运动有关的晚新元古代群体(640-550 Ma)和与Gondwanides造山运动有关的二叠纪-三叠纪群体(280-200 Ma)。在~ 960 Ma和~ 345 Ma也有两个小簇。年龄在1000 ~ 200 Ma之间的锆石颗粒在反复的地壳改造过程中结晶,其特征是在640 ~ 510 Ma高度演化的εHf(t)特征(−10 ~−30),表明古亚马逊河克拉通的来源,没有潘潘纪或法马提纪贡献的证据。石炭世(380 ~ 310 Ma)幼岩输入显著增加,其后以大陆输入为主,δ18O值持续高至220 Ma。虽然这些样品的U-Pb年龄谱与安第斯山脉中部相似,但同位素和地球化学数据显示,安第斯山脉中北部边缘的构造背景与冈瓦纳山脉中东部(即非洲中部和南美洲东部)更为接近,而不是典型的安第斯山脉背景。
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来源期刊
Journal of South American Earth Sciences
Journal of South American Earth Sciences 地学-地球科学综合
CiteScore
3.70
自引率
22.20%
发文量
364
审稿时长
6-12 weeks
期刊介绍: Papers must have a regional appeal and should present work of more than local significance. Research papers dealing with the regional geology of South American cratons and mobile belts, within the following research fields: -Economic geology, metallogenesis and hydrocarbon genesis and reservoirs. -Geophysics, geochemistry, volcanology, igneous and metamorphic petrology. -Tectonics, neo- and seismotectonics and geodynamic modeling. -Geomorphology, geological hazards, environmental geology, climate change in America and Antarctica, and soil research. -Stratigraphy, sedimentology, structure and basin evolution. -Paleontology, paleoecology, paleoclimatology and Quaternary geology. New developments in already established regional projects and new initiatives dealing with the geology of the continent will be summarized and presented on a regular basis. Short notes, discussions, book reviews and conference and workshop reports will also be included when relevant.
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