Detrital zircon U-Pb and Hf isotope signature of Carboniferous and older strata of the Yukon-Tanana terrane in Yukon, Canadian Cordillera: Implications for terrane correlations and the onset of Late Devonian arc magmatism

IF 1.7 3区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Geosphere Pub Date : 2023-05-19 DOI:10.1130/ges02607.1
E. Kroeger, W. McClelland, M. Colpron, S. Piercey, G. Gehrels
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Abstract

The Yukon-Tanana terrane in Yukon, Canada, records Late Devonian (ca. 366–360 Ma) rifting and the onset of latest Devonian–Carboniferous arc and back-arc magmatism (ca. 360–325 Ma) in the Northern Cordillera. Detrital zircon U-Pb and Hf isotope analyses indicate that the metasedimentary basement of the Yukon-Tanana terrane was sourced in northwestern Laurentia. Sandstones in Late Devonian–Carboniferous successions generally have robust Late Devonian–Mississippian age peaks, and their Hf isotope signatures are characterized by strongly negative εHft values in Late Devonian zircons followed by progressively more juvenile εHft values in Carboniferous zircons. This Hf isotopic “pull-up” reflects the melting of Precambrian crust related to regional extension in the Late Devonian, followed by progressively more juvenile magmatism as the arc matured through the Carboniferous. Paleozoic rocks of the Tracy Arm terrane in southeastern Alaska, USA (formerly Yukon-Tanana south), have been compared with the Yukon-Tanana terrane in Yukon. Detrital zircons from the metasedimentary basement to the Tracy Arm terrane have distinct Precambrian populations that indicate sources along a different segment of the Laurentian margin compared to basement of the Yukon-Tanana terrane. Magmatism in the Tracy Arm terrane ranges from 440 Ma to 360 Ma and is characterized by an Hf isotopic “pull-down” in the Silurian to Early Devonian, followed by a “pull-up” in the Middle to Late Devonian and a second “pull-down” in the Late Devonian to early Mississippian. Thus, the Yukon-Tanana and Tracy Arm terranes record distinct pre-Carboniferous histories. Interactions between these two terranes are suggested by the influx of exotic early Mississippian clasts and detrital zircons on the Tracy Arm terrane that match sources in the Yukon-Tanana terrane.
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加拿大育空地区石炭系及更老地层碎屑锆石U-Pb和Hf同位素特征:地表对比与晚泥盆世弧岩浆活动的意义
加拿大育空地区的育空-塔纳那地体记录了晚泥盆纪(约366–360 Ma)的裂谷作用以及北科迪勒拉地区最新泥盆纪-石炭纪弧和弧后岩浆作用的开始(约360–325 Ma)。碎屑锆石U-Pb和Hf同位素分析表明,育空-塔纳地体的变质沉积基底来源于劳伦西北部。晚泥盆纪-石炭纪序列中的砂岩通常具有强大的晚泥盆世-密西西比时代峰值,其Hf同位素特征是晚泥盆统锆石中的εHft值为强负,随后石炭纪锆石中的δHft值逐渐增加。这种Hf同位素“上拉”反映了与晚泥盆纪区域伸展有关的前寒武纪地壳的融化,随后随着弧在石炭纪成熟,出现了越来越多的年轻岩浆活动。美国阿拉斯加州东南部Tracy Arm地体(前育空-塔纳南部)的古生代岩石已与育空地区的育空-塔那纳地体进行了比较。从变质沉积基底到Tracy Arm地体的碎屑锆石具有不同的前寒武纪种群,这表明与育空-塔纳地体基底相比,劳伦阶边缘的不同段存在来源。Tracy Arm地体的岩浆作用范围从440 Ma到360 Ma,其特征是志留纪到早泥盆纪的Hf同位素“下拉”,随后在中泥盆纪到晚泥盆纪发生“上拉”,在晚泥盆世到早密西西比纪发生第二次“下拉”。因此,育空-塔纳纳地体和特蕾西-阿姆地体记录了不同的前石炭世历史。Tracy Arm地体上外来的早期密西西比碎屑和碎屑锆石的流入表明了这两个地体之间的相互作用,这些碎屑和锆石与育空-塔纳那地体的来源相匹配。
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来源期刊
Geosphere
Geosphere 地学-地球科学综合
CiteScore
4.40
自引率
12.00%
发文量
71
审稿时长
6-12 weeks
期刊介绍: Geosphere is GSA''s ambitious, online-only publication that addresses the growing need for timely publication of research results, data, software, and educational developments in ways that cannot be addressed by traditional formats. The journal''s rigorously peer-reviewed, high-quality research papers target an international audience in all geoscience fields. Its innovative format encourages extensive use of color, animations, interactivity, and oversize figures (maps, cross sections, etc.), and provides easy access to resources such as GIS databases, data archives, and modeling results. Geosphere''s broad scope and variety of contributions is a refreshing addition to traditional journals.
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