Lichen Hu , Ning Li , Xiaowei Fu , Xianjun Tang , Kailong Feng , Weilin Zhu , Xi Xu
{"title":"揭示华南~ 110 Ma大陆弧:来自东海盆地近海岩浆记录的地球化学和同位素信息","authors":"Lichen Hu , Ning Li , Xiaowei Fu , Xianjun Tang , Kailong Feng , Weilin Zhu , Xi Xu","doi":"10.1016/j.gr.2025.03.013","DOIUrl":null,"url":null,"abstract":"<div><div>The rollback of the paleo-Pacific plate is widely believed to have driven the trenchward migration of the magmatic belt in South China (SC) during the Early Cretaceous. However, the lack of arc andesite and the apparent cessation of magmatism between 117 and 108 Ma in the onshore region has sparked debates regarding the tectonic models. Notably, magmatism in the offshore East China Sea Basin (ECSB) has been largely overlooked. This study presents a comprehensive analysis of 21 magmatic rock samples from 10 industrial wells in the ECSB. Through thin-section petrography, in situ zircon U–Pb dating, Hf isotopes, and whole-rock geochemical analyses, we identified these samples as granites, andesites and tuff with ages of ∼110 Ma (107.9–112.9 Ma). The samples are enriched in large ion lithophile elements (LILEs, such as Ba, K, Pb, Sr, and Nd), and depleted in high field strength elements (HFSEs, like Nb, Ta, P, and Ti) and light rare earth elements (LREEs), with no Eu anomalies observed. All the granites are I-type granites, characterized by low CaO (0.8–2.8 %) and high Na<sub>2</sub>O (3.7–4.6 %) contents, as well as low Nb, Rb, Y, Yb, and Ta contents, suggesting a volcanic arc tectonic setting. The andesites, formed in a continental arc environment, as suggested by their low Sc contents (3.3 ∼ 15.3 ppm). Zircon Hf isotopes show slightly negative ε<sub>Hf</sub>(t) values (−0.1 to −6.3), which contrast with the more negative onshore values (−5 to −10), indicating a higher contribution of mantle-derived material in the offshore magmatic rocks. Collectively, these data suggest the existence of a ∼110 Ma continental arc extending from NE Fujian to the ECSB, which underwent significant clockwise rotation relative to earlier onshore arcs. We propose that asynchronous rollback of the paleo-Pacific plate facilitated the eastward migration of this arc, while placing onshore South China in a back-arc tectonic setting during ∼110 Ma.</div></div>","PeriodicalId":12761,"journal":{"name":"Gondwana Research","volume":"143 ","pages":"Pages 239-255"},"PeriodicalIF":7.2000,"publicationDate":"2025-04-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Unveiling the ∼110 Ma continental arc in South China: geochemical and isotopic insights from offshore magmatic records in the East China Sea Basin\",\"authors\":\"Lichen Hu , Ning Li , Xiaowei Fu , Xianjun Tang , Kailong Feng , Weilin Zhu , Xi Xu\",\"doi\":\"10.1016/j.gr.2025.03.013\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>The rollback of the paleo-Pacific plate is widely believed to have driven the trenchward migration of the magmatic belt in South China (SC) during the Early Cretaceous. However, the lack of arc andesite and the apparent cessation of magmatism between 117 and 108 Ma in the onshore region has sparked debates regarding the tectonic models. Notably, magmatism in the offshore East China Sea Basin (ECSB) has been largely overlooked. This study presents a comprehensive analysis of 21 magmatic rock samples from 10 industrial wells in the ECSB. Through thin-section petrography, in situ zircon U–Pb dating, Hf isotopes, and whole-rock geochemical analyses, we identified these samples as granites, andesites and tuff with ages of ∼110 Ma (107.9–112.9 Ma). The samples are enriched in large ion lithophile elements (LILEs, such as Ba, K, Pb, Sr, and Nd), and depleted in high field strength elements (HFSEs, like Nb, Ta, P, and Ti) and light rare earth elements (LREEs), with no Eu anomalies observed. All the granites are I-type granites, characterized by low CaO (0.8–2.8 %) and high Na<sub>2</sub>O (3.7–4.6 %) contents, as well as low Nb, Rb, Y, Yb, and Ta contents, suggesting a volcanic arc tectonic setting. The andesites, formed in a continental arc environment, as suggested by their low Sc contents (3.3 ∼ 15.3 ppm). Zircon Hf isotopes show slightly negative ε<sub>Hf</sub>(t) values (−0.1 to −6.3), which contrast with the more negative onshore values (−5 to −10), indicating a higher contribution of mantle-derived material in the offshore magmatic rocks. Collectively, these data suggest the existence of a ∼110 Ma continental arc extending from NE Fujian to the ECSB, which underwent significant clockwise rotation relative to earlier onshore arcs. We propose that asynchronous rollback of the paleo-Pacific plate facilitated the eastward migration of this arc, while placing onshore South China in a back-arc tectonic setting during ∼110 Ma.</div></div>\",\"PeriodicalId\":12761,\"journal\":{\"name\":\"Gondwana Research\",\"volume\":\"143 \",\"pages\":\"Pages 239-255\"},\"PeriodicalIF\":7.2000,\"publicationDate\":\"2025-04-26\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Gondwana Research\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S1342937X25001078\",\"RegionNum\":1,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"GEOSCIENCES, MULTIDISCIPLINARY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Gondwana Research","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S1342937X25001078","RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
Unveiling the ∼110 Ma continental arc in South China: geochemical and isotopic insights from offshore magmatic records in the East China Sea Basin
The rollback of the paleo-Pacific plate is widely believed to have driven the trenchward migration of the magmatic belt in South China (SC) during the Early Cretaceous. However, the lack of arc andesite and the apparent cessation of magmatism between 117 and 108 Ma in the onshore region has sparked debates regarding the tectonic models. Notably, magmatism in the offshore East China Sea Basin (ECSB) has been largely overlooked. This study presents a comprehensive analysis of 21 magmatic rock samples from 10 industrial wells in the ECSB. Through thin-section petrography, in situ zircon U–Pb dating, Hf isotopes, and whole-rock geochemical analyses, we identified these samples as granites, andesites and tuff with ages of ∼110 Ma (107.9–112.9 Ma). The samples are enriched in large ion lithophile elements (LILEs, such as Ba, K, Pb, Sr, and Nd), and depleted in high field strength elements (HFSEs, like Nb, Ta, P, and Ti) and light rare earth elements (LREEs), with no Eu anomalies observed. All the granites are I-type granites, characterized by low CaO (0.8–2.8 %) and high Na2O (3.7–4.6 %) contents, as well as low Nb, Rb, Y, Yb, and Ta contents, suggesting a volcanic arc tectonic setting. The andesites, formed in a continental arc environment, as suggested by their low Sc contents (3.3 ∼ 15.3 ppm). Zircon Hf isotopes show slightly negative εHf(t) values (−0.1 to −6.3), which contrast with the more negative onshore values (−5 to −10), indicating a higher contribution of mantle-derived material in the offshore magmatic rocks. Collectively, these data suggest the existence of a ∼110 Ma continental arc extending from NE Fujian to the ECSB, which underwent significant clockwise rotation relative to earlier onshore arcs. We propose that asynchronous rollback of the paleo-Pacific plate facilitated the eastward migration of this arc, while placing onshore South China in a back-arc tectonic setting during ∼110 Ma.
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''.