2.7-Ga-old mafic dike in the Trans-North China Orogen of the North China Craton and its tectonic significance-Reference-Cited by-同舟云学术

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2.7-Ga-old mafic dike in the Trans-North China Orogen of the North China Craton and its tectonic significance

Published:2023-09-19 Issue:6 Volume:42 Page:1124-1129
ISSN:2096-0956
Container-title:Acta Geochimica
language:en
Short-container-title:Acta Geochim

Author:

Liu Haiyan,Peng Chong^ORCID

Funder

Key Laboratory of Deep-Earth Dynamics of Ministry of Natural Resources, Institute of Geology, Chinese Academy of Geological Sciences

Education Department of Shanxi Province

Shanxi Normal University

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology

Link

https://link.springer.com/content/pdf/10.1007/s11631-023-00638-2.pdf

Reference30 articles.

1. Belousova E, Griffin W, O’Reilly SY, Fisher N (2002) Igneous zircon: trace element composition as an indicator of source rock type. Contrib Miner Petrol 143(5):602–622

2. Buchan KL et al (2001) Rodinia: the evidence from integrated paleomagnetism and U-Pb geochronology. Precambr Res 110(1):9–32

3. Condie KC (1989) Geochemical changes in basalts and andesites across the Archean-Proterozoic boundary: identification and significance. Lithos 23(1–2):1–18

4. Ernst R, Srivastava R, Bleeker W, Hamilton M (2010) Precambrian Large Igneous Provinces (LIPs) and their dyke swarms: new insights from high-precision geochronology integrated with paleomagnetism and geochemistry. Precambr Res 183(3):vii–xi

5. Floyd PA, Winchester JA (1975) Magma type and tectonic setting discrimination using immobile elements. Earth Planet Sci Lett 27(2):211–218

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