华东地质2026，Vol.47Issue(1)：72-81,10.DOI:10.16788/j.hddz.32-1865/P.2025.02.002
扬子陆核古元古代构造-岩浆演化
Paleoproterozoic tectonic-magmatic evolution in the nucleus of the Yangtze Craton
摘要
Abstract
The Huangling Dome exposed in the nucleus of the Yangtze Craton is an ideal window for ex-ploring the formation and evolution in the Precambrian continental crust of the craton.This paper summarized the research achievement on zircon U-Pb geochronology,Hf isotope and geochemical features of the Paleoprotero-zoic magmatic rocks in the nucleus of the Yangtze Craton,and discussed the nature,petrogenesis and tectonic set-ting of these rocks,so as to constrain the geodynamic and tectonic evolution processes in the nucleus of the Yangtze Craton during Paleoproterozoic.It is concluded that the Paleoproterozoic tectonic-magmatic evolution can be divided into four processes,namely the subduction and accretion,uplift and erosion,high-grade metamor-phism,and orogenic collapse,which are associated with three stages:oceanic subduction,arc-continent collision,and post-collisional extension.关键词
扬子陆核/古元古代/地壳演化/构造-岩浆过程Key words
nucleus of the Yangtze Craton/Paleoproterozoic/crustal evolution/tectonic-magmatic processes分类
天文与地球科学引用本文复制引用
邱啸飞,魏运许,赵小明,徐扬,田洋,徐大良,卢山松,邓新,彭练红..扬子陆核古元古代构造-岩浆演化[J].华东地质,2026,47(1):72-81,10.基金项目
国家自然科学基金"北大别始太古代基底岩系的组成、地球化学特征及其对早期地壳演化的制约(编号:42272229)""中国三大克拉通太古宙陆壳的形成演化和构造机制(编号:U2344210)"和武汉地质调查中心潜龙人才基金"北大别太古宙早期TTG片麻岩锆石中磷灰石包裹体的Sr同位素组成及其对早期地壳演化的指示(编号:QL2022-02)"项目联合资助. （编号:42272229）
