Yuejun Wang , Yuebiao Wu , Xin Qian , Peter A. Cawood , Jiaxin Zhu , Tianxing Bai , Cheng Wang , Yang Xu
{"title":"婆罗洲中部的古元古代变质基底:连接印度支那和哥伦比亚的劳伦西亚","authors":"Yuejun Wang , Yuebiao Wu , Xin Qian , Peter A. Cawood , Jiaxin Zhu , Tianxing Bai , Cheng Wang , Yang Xu","doi":"10.1016/j.gr.2025.07.004","DOIUrl":null,"url":null,"abstract":"<div><div>Zircon U-Pb geochronological and Lu-Hf isotopic data, combined with whole-rock geochemical and Sr-Nd-Pb isotopic results for metamorphic rocks from the Embuoi Complex and associated massive granites, SE Asia, document the Precambrian tectonic evolution of this region and constrain its relationship to Laurentia in the Columbia supercontinent. Plagioclase amphibolite, orthogneiss and paragneiss from the Embuoi Complex yield zircon U-Pb ages in the range of 1898–1820 Ma, representing the oldest known rocks in Borneo. The Embuoi plagioclase amphibolite exhibits the arc-like geochemical signatures with ε<sub>Nd</sub>(t) = +2.4–+6.7, (<sup>206</sup>Pb/<sup>204</sup>Pb)<sub>i</sub> = 18.75–19.11, (<sup>207</sup>Pb/<sup>204</sup>Pb)<sub>i</sub> = 15.65–15.75 and (<sup>208</sup>Pb/<sup>204</sup>Pb)<sub>i</sub> = 38.51–39.31, suggesting the derivation from a MORB-like source modified by input of the subduction-related components. Orthogneisses have affinity to A<sub>2</sub> granite and originated by Neoarchean–Paleoproterozoic crustal anatexis in a post-collisional setting. The ca. 1.85 Ga paragneiss shares comparable zircon ε<sub>Hf</sub>(t) and T<sup>Hf</sup><sub>DM</sub> values and consistent Sr-Nd-Pb isotopes with the coeval orthogneiss, suggesting proximal derivation from a Paleoproterozoic felsic source. Rocks of the complex record development of a Paleoproterozoic Embuoi orogeny on the foundation of Archaean crust. Integration of available data from the adjacent blocks in SE Asia with those from Laurentia suggests the tectonic affinity of the Embuoi fragment with the Indochina block, positioning them both as the western extension of SW Laurentia within the Columbia supercontinent. The Paleoproterozoic Embuoi orogeny was overprinted by Triassic (259–201 Ma) metamorphism and intruded by Triassic (233–211 Ma) massive granites that correlate with Paleo-Pacific subduction along the East Asia active continental margin. These findings establish the Precambrian basement architecture of Borneo and underscore its significance in Columbia’s assembly and Triassic Paleo-Pacific active margin dynamics.</div></div>","PeriodicalId":12761,"journal":{"name":"Gondwana Research","volume":"148 ","pages":"Pages 77-95"},"PeriodicalIF":7.2000,"publicationDate":"2025-07-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Paleoproterozoic metamorphic basement in Central Borneo: linking Indochina and Laurentia in Columbia\",\"authors\":\"Yuejun Wang , Yuebiao Wu , Xin Qian , Peter A. Cawood , Jiaxin Zhu , Tianxing Bai , Cheng Wang , Yang Xu\",\"doi\":\"10.1016/j.gr.2025.07.004\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>Zircon U-Pb geochronological and Lu-Hf isotopic data, combined with whole-rock geochemical and Sr-Nd-Pb isotopic results for metamorphic rocks from the Embuoi Complex and associated massive granites, SE Asia, document the Precambrian tectonic evolution of this region and constrain its relationship to Laurentia in the Columbia supercontinent. Plagioclase amphibolite, orthogneiss and paragneiss from the Embuoi Complex yield zircon U-Pb ages in the range of 1898–1820 Ma, representing the oldest known rocks in Borneo. The Embuoi plagioclase amphibolite exhibits the arc-like geochemical signatures with ε<sub>Nd</sub>(t) = +2.4–+6.7, (<sup>206</sup>Pb/<sup>204</sup>Pb)<sub>i</sub> = 18.75–19.11, (<sup>207</sup>Pb/<sup>204</sup>Pb)<sub>i</sub> = 15.65–15.75 and (<sup>208</sup>Pb/<sup>204</sup>Pb)<sub>i</sub> = 38.51–39.31, suggesting the derivation from a MORB-like source modified by input of the subduction-related components. Orthogneisses have affinity to A<sub>2</sub> granite and originated by Neoarchean–Paleoproterozoic crustal anatexis in a post-collisional setting. The ca. 1.85 Ga paragneiss shares comparable zircon ε<sub>Hf</sub>(t) and T<sup>Hf</sup><sub>DM</sub> values and consistent Sr-Nd-Pb isotopes with the coeval orthogneiss, suggesting proximal derivation from a Paleoproterozoic felsic source. Rocks of the complex record development of a Paleoproterozoic Embuoi orogeny on the foundation of Archaean crust. Integration of available data from the adjacent blocks in SE Asia with those from Laurentia suggests the tectonic affinity of the Embuoi fragment with the Indochina block, positioning them both as the western extension of SW Laurentia within the Columbia supercontinent. The Paleoproterozoic Embuoi orogeny was overprinted by Triassic (259–201 Ma) metamorphism and intruded by Triassic (233–211 Ma) massive granites that correlate with Paleo-Pacific subduction along the East Asia active continental margin. 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Paleoproterozoic metamorphic basement in Central Borneo: linking Indochina and Laurentia in Columbia
Zircon U-Pb geochronological and Lu-Hf isotopic data, combined with whole-rock geochemical and Sr-Nd-Pb isotopic results for metamorphic rocks from the Embuoi Complex and associated massive granites, SE Asia, document the Precambrian tectonic evolution of this region and constrain its relationship to Laurentia in the Columbia supercontinent. Plagioclase amphibolite, orthogneiss and paragneiss from the Embuoi Complex yield zircon U-Pb ages in the range of 1898–1820 Ma, representing the oldest known rocks in Borneo. The Embuoi plagioclase amphibolite exhibits the arc-like geochemical signatures with εNd(t) = +2.4–+6.7, (206Pb/204Pb)i = 18.75–19.11, (207Pb/204Pb)i = 15.65–15.75 and (208Pb/204Pb)i = 38.51–39.31, suggesting the derivation from a MORB-like source modified by input of the subduction-related components. Orthogneisses have affinity to A2 granite and originated by Neoarchean–Paleoproterozoic crustal anatexis in a post-collisional setting. The ca. 1.85 Ga paragneiss shares comparable zircon εHf(t) and THfDM values and consistent Sr-Nd-Pb isotopes with the coeval orthogneiss, suggesting proximal derivation from a Paleoproterozoic felsic source. Rocks of the complex record development of a Paleoproterozoic Embuoi orogeny on the foundation of Archaean crust. Integration of available data from the adjacent blocks in SE Asia with those from Laurentia suggests the tectonic affinity of the Embuoi fragment with the Indochina block, positioning them both as the western extension of SW Laurentia within the Columbia supercontinent. The Paleoproterozoic Embuoi orogeny was overprinted by Triassic (259–201 Ma) metamorphism and intruded by Triassic (233–211 Ma) massive granites that correlate with Paleo-Pacific subduction along the East Asia active continental margin. These findings establish the Precambrian basement architecture of Borneo and underscore its significance in Columbia’s assembly and Triassic Paleo-Pacific active margin dynamics.
期刊介绍:
Gondwana Research (GR) is an International Journal aimed to promote high quality research publications on all topics related to solid Earth, particularly with reference to the origin and evolution of continents, continental assemblies and their resources. GR is an "all earth science" journal with no restrictions on geological time, terrane or theme and covers a wide spectrum of topics in geosciences such as geology, geomorphology, palaeontology, structure, petrology, geochemistry, stable isotopes, geochronology, economic geology, exploration geology, engineering geology, geophysics, and environmental geology among other themes, and provides an appropriate forum to integrate studies from different disciplines and different terrains. In addition to regular articles and thematic issues, the journal invites high profile state-of-the-art reviews on thrust area topics for its column, ''GR FOCUS''. Focus articles include short biographies and photographs of the authors. Short articles (within ten printed pages) for rapid publication reporting important discoveries or innovative models of global interest will be considered under the category ''GR LETTERS''.