赞皇地体糜棱岩<sup>39</sup>Ar-<sup>40</sup>Ar年代学及EBSD组构分析：对华北克拉通古元古代构造热演化过程的启示

吕涛; 蒋康; 王军鹏; 焦韵哲; 翟磊

doi:10.3799/dqkx.2022.359

Volume 50 Issue 4

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Article Navigation > Earth Science > 2025 > 50(4): 1273-1283

Lü Tao, Jiang Kang, Wang Junpeng, Jiao Yunzhe, Zhai Lei, 2025. 39Ar-40Ar Geochronology and EBSD Analysis of Mylonite in Zanhuang Massif: Implications for Paleoproterozoic Tectono-Thermal Evolution of North China Craton. Earth Science, 50(4): 1273-1283. doi: 10.3799/dqkx.2022.359

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Lü Tao, Jiang Kang, Wang Junpeng, Jiao Yunzhe, Zhai Lei, 2025. ³⁹Ar-⁴⁰Ar Geochronology and EBSD Analysis of Mylonite in Zanhuang Massif: Implications for Paleoproterozoic Tectono-Thermal Evolution of North China Craton. Earth Science, 50(4): 1273-1283. doi: 10.3799/dqkx.2022.359

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³⁹Ar-⁴⁰Ar Geochronology and EBSD Analysis of Mylonite in Zanhuang Massif: Implications for Paleoproterozoic Tectono-Thermal Evolution of North China Craton

doi: 10.3799/dqkx.2022.359

Lü Tao^{1
,
,},
Jiang Kang¹,
Wang Junpeng^{1
,
,
,},
Jiao Yunzhe¹,
Zhai Lei²

1.
School of Earth Sciences, China University of Geosciences (Wuhan), Wuhan 430074, China
2.
CCCC-SHB Fourth Engineering Co., Ltd., Luoyang 471013, China

Received Date: 2022-08-28
Available Online: 2025-05-10
Publish Date: 2025-04-25

Abstract

Abstract

The Zanhuang massif is located in the southeast part of the Central Orogenic Belt of the North China Craton, with complex rock association and tectonic deformation from Archaean to Paleoproterozoic. It is important to study the Early Precambrian tectono-thermal evolution of the Central Orogenic Belt of the North China Craton. In this study, a large-scale rock structure mapping, petrography, biotite ³⁹Ar-⁴⁰Ar geochronology and quartz EBSD fabric analysis of a well-out cropping ductile shear zone in the Zanhuang massif were carried out to define the kinematic characteristics and formation age of the shear zone, and to further explore the Paleoproterozoic tectono-thermal evolution of the North China Craton. The main lithology of the ductile shear zone is granitic mylonite, mainly composed of quartz (30%-40%), biotite (5%-15%) and feldspar (35%-55%). In the study area, the rocks are strongly deformed and metamorphosed, and a series of normal faults, folds, lineaments, foliations, and rotated porphyroblasts are developed. The surface occurrence and the trail of rotating patches all indicate the NW-SE shear. A plateau age of 1 781-1 745 Ma for biotite in mylonite was obtained by argon age test, indicating that the shear zone was formed in the Late Paleoproterozoic. EBSD fabric of quartz in mylonite shows that the quartz is mainly underside a-slip, indicating that the deformation temperature is lower than 400 ℃. Based on the previous research results, this study shows that the Zanhuang metamorphic complex experienced a strong disturbance caused by a tectono-thermal event in the Late Paleoproterozoic.
- Paleoproterozoic,
- mylonite,
- ³⁹Ar-⁴⁰Ar dating,
- tectono-thermal evolution,
- Zanhuang massif,
- North China Craton,
- structural geology

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References(54)

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39Ar-40Ar Geochronology and EBSD Analysis of Mylonite in Zanhuang Massif: Implications for Paleoproterozoic Tectono-Thermal Evolution of North China Craton

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³⁹Ar-⁴⁰Ar Geochronology and EBSD Analysis of Mylonite in Zanhuang Massif: Implications for Paleoproterozoic Tectono-Thermal Evolution of North China Craton