Metamorphic and chronological constraints on the early Paleozoic tectono-thermal evolution of the Olkhon Terrane, southern Siberia

IF 3.5 2区 地球科学 Q1 GEOLOGY Journal of Metamorphic Geology Pub Date : 2022-12-22 DOI:10.1111/jmg.12706
Zhiyong Li, Yingde Jiang, Stephen Collett, Pavla Štípská, Karel Schulmann, Sheng Wang, Vasiliy Sukhorukov
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引用次数: 2

Abstract

Terranes accreted to the southeastern margin of the Siberian Craton record an important early Paleozoic tectono-thermal event (known as the Baikal orogenic cycle) in the evolution of the Central Asian Orogenic Belt (CAOB). However, the precise metamorphic conditions and relative timing of this event and its linkage to the wider CAOB remain far poorly constrained. The best exposed of these terranes is the Olkhon Terrane on the western bank of Lake Baikal. Here, late Neoproterozoic through early Paleozoic island arc and back-arc assemblages were metamorphosed to form a thin granulite facies belt cropping out adjacent to the Siberian Craton and lower temperature/pressure paragneiss and migmatite towards the southeast. Phase equilibria modelling suggests that the granulite facies belt preserved moderate pressure (c. 0.80 GPa) and high temperature (up to 900°C) conditions while the paragneiss and migmatites in the southeast have peak metamorphic conditions around 700–770°C at 0.60–0.80 GPa. New geochronological data (zircon U–Pb in granulite and monazite U–Pb in paragneiss/migmatite) in combination with phase equilibria modelling and petro-structural analysis suggest that the tectono-metamorphic evolution of the Olkhon Terrane was controlled by a long-lasting (535–450 Ma) and pervasive thermal anomaly. Discrete maxima in the zircon and monazite U–Pb ages at c. 535, 500, and 450 Ma are linked to different stages of a semi-continuous high-temperature metamorphic evolution. Based on existing geological data of the region, a generalized geodynamic model for the Baikal orogenic cycle involving switching between compressional and extensional regimes during the early Paleozoic accretion of ‘exotic’ CAOB-derived material to the southern margin of Siberia is proposed. The tectono-metamorphic evolution of the Olkhon Terrane may represent a world-class example of polyphase shortening of a long-lived hot intra-continental arc–back-arc system during its collision with cratonic blocks.

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西伯利亚南部Olkhon地体早古生代构造-热演化的变质和年代学约束
西伯利亚克拉通东南缘的地体增生记录了中亚造山带(CAOB)演化过程中一个重要的早古生代构造-热事件(即贝加尔湖造山带旋回)。然而,这一事件的精确变质条件和相对时间以及它与更广泛的CAOB的联系仍然知之甚少。这些岩层中暴露得最好的是贝加尔湖西岸的奥尔洪岩层。晚新元古代至早古生代岛弧和弧后组合变质,形成一条细麻粒岩相带,与西伯利亚克拉通相邻,东南方向为低温/低压副长岩和混辉岩。相平衡模拟表明,麻粒岩相带保持了中压(约0.80 GPa)和高温(高达900℃)条件,而东南部的副长岩和混辉岩则在0.60 ~ 0.80 GPa时处于700 ~ 770℃左右的峰值变质条件。新的年代学数据(麻粒岩中的锆石U-Pb和副长岩/混辉岩中的独一石U-Pb)结合相平衡模拟和石油构造分析表明,奥尔洪地体的构造变质演化是由一个长期(535-450 Ma)和普遍的热异常控制的。锆石和独居石U-Pb年龄在535、500和450 Ma的离散最大值与半连续高温变质演化的不同阶段有关。基于该地区现有的地质资料,提出了一个贝加尔湖造山旋回的广义地球动力学模型,该模型涉及早古生代“外来”CAOB衍生物质向西伯利亚南缘增生期间挤压和伸展状态之间的转换。奥尔洪地体的构造变质演化可能代表了在与克拉通地块碰撞过程中,一个长期存在的热大陆内弧-弧后体系的多期缩短的世界级例子。
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来源期刊
CiteScore
6.60
自引率
11.80%
发文量
57
审稿时长
6-12 weeks
期刊介绍: The journal, which is published nine times a year, encompasses the entire range of metamorphic studies, from the scale of the individual crystal to that of lithospheric plates, including regional studies of metamorphic terranes, modelling of metamorphic processes, microstructural and deformation studies in relation to metamorphism, geochronology and geochemistry in metamorphic systems, the experimental study of metamorphic reactions, properties of metamorphic minerals and rocks and the economic aspects of metamorphic terranes.
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