Ferrodoleritic dykes in the Tarim Craton signal Neoproterozoic breakup of Rodinia supercontinent
[Display omitted] •We provide the first description of the rarely ferrodoleritic dykes in the Neoproterozoic Tarim Craton.•The ferrodolerites were derived from a mixed mantle source of garnet lherzolite and pyroxenite.•The ferrodoleritic dykes record the onset of Rodinia supercontinent breakup. Mafi...
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| Published in | Journal of Asian earth sciences Vol. 200; p. 104476 |
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| Main Authors | , , , , , , |
| Format | Journal Article |
| Language | English |
| Published |
Elsevier Ltd
15.09.2020
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| Subjects | |
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| Abstract | [Display omitted]
•We provide the first description of the rarely ferrodoleritic dykes in the Neoproterozoic Tarim Craton.•The ferrodolerites were derived from a mixed mantle source of garnet lherzolite and pyroxenite.•The ferrodoleritic dykes record the onset of Rodinia supercontinent breakup.
Mafic dyke swarms are important bar codes for the rifting and breakup of supercontinents. Here we report a Neoproterozoic mafic (ferrodoleritic) dyke swarm from the Aksu area along the northern margin of the Tarim Craton, NW China. Zircon U-Pb analyses of two dyke samples yielded ages of 801 ± 9 Ma and 804 ± 13 Ma. The ferrodoleritic dykes show high total FeO (11.55–14.55 wt%) and TiO2 contents (2.84–3.26 wt%) and variable SiO2 (47.90–52.74 wt%). They display positive anomalies of Rb, Ba, K and negative anomalies of Nb, Ta, Ti and the enrichment of light rare earth elements relative to heavy rare earth elements. The whole-rock εNd(t) values (–5.4 to –7.2) indicate a relatively homogeneous and enriched magma source. Trace element modelling suggests that the ferrodoleritic dykes were generated by low degree of partial melting (garnet lherzolite 3–5%, pyroxenite 5–10%) of a mixed mantle source (60% garnet lherzolite and 40% pyroxenite). The results from our study suggest two major mafic magma pulses at ca. 830–800 Ma and ca. 780–750 Ma during the Neoproterozoic, which we correlate to the onset of Rodinia supercontinent breakup. |
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| AbstractList | [Display omitted]
•We provide the first description of the rarely ferrodoleritic dykes in the Neoproterozoic Tarim Craton.•The ferrodolerites were derived from a mixed mantle source of garnet lherzolite and pyroxenite.•The ferrodoleritic dykes record the onset of Rodinia supercontinent breakup.
Mafic dyke swarms are important bar codes for the rifting and breakup of supercontinents. Here we report a Neoproterozoic mafic (ferrodoleritic) dyke swarm from the Aksu area along the northern margin of the Tarim Craton, NW China. Zircon U-Pb analyses of two dyke samples yielded ages of 801 ± 9 Ma and 804 ± 13 Ma. The ferrodoleritic dykes show high total FeO (11.55–14.55 wt%) and TiO2 contents (2.84–3.26 wt%) and variable SiO2 (47.90–52.74 wt%). They display positive anomalies of Rb, Ba, K and negative anomalies of Nb, Ta, Ti and the enrichment of light rare earth elements relative to heavy rare earth elements. The whole-rock εNd(t) values (–5.4 to –7.2) indicate a relatively homogeneous and enriched magma source. Trace element modelling suggests that the ferrodoleritic dykes were generated by low degree of partial melting (garnet lherzolite 3–5%, pyroxenite 5–10%) of a mixed mantle source (60% garnet lherzolite and 40% pyroxenite). The results from our study suggest two major mafic magma pulses at ca. 830–800 Ma and ca. 780–750 Ma during the Neoproterozoic, which we correlate to the onset of Rodinia supercontinent breakup. |
| ArticleNumber | 104476 |
| Author | Wang, Zhenchao Zhang, Qiang Liu, Linghan Zhang, Zhaochong Santosh, M. Jin, Shengkai Li, Hengxu |
| Author_xml | – sequence: 1 givenname: Hengxu surname: Li fullname: Li, Hengxu organization: State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China – sequence: 2 givenname: Zhaochong orcidid: 0000-0002-5798-3285 surname: Zhang fullname: Zhang, Zhaochong email: zczhang@cugb.edu.cn organization: State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China – sequence: 3 givenname: M. orcidid: 0000-0002-1073-8477 surname: Santosh fullname: Santosh, M. organization: State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China – sequence: 4 givenname: Zhenchao surname: Wang fullname: Wang, Zhenchao organization: State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China – sequence: 5 givenname: Shengkai surname: Jin fullname: Jin, Shengkai organization: State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China – sequence: 6 givenname: Qiang surname: Zhang fullname: Zhang, Qiang organization: State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China – sequence: 7 givenname: Linghan orcidid: 0000-0001-6519-4545 surname: Liu fullname: Liu, Linghan organization: State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China |
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| CitedBy_id | crossref_primary_10_3390_min13111446 crossref_primary_10_1016_j_palaeo_2024_112404 crossref_primary_10_1130_B36305_1 crossref_primary_10_1016_j_palaeo_2024_112662 crossref_primary_10_1016_j_lithos_2021_106156 crossref_primary_10_1002_gj_5132 crossref_primary_10_18654_1000_0569_2021_08_12 crossref_primary_10_1016_j_precamres_2023_107110 crossref_primary_10_1080_00206814_2022_2129474 |
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•We provide the first description of the rarely ferrodoleritic dykes in the Neoproterozoic Tarim Craton.•The ferrodolerites were derived from... |
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| SubjectTerms | Ferrodolerites Petrogenesis Rodinia supercontinent Tarim Craton |
| Title | Ferrodoleritic dykes in the Tarim Craton signal Neoproterozoic breakup of Rodinia supercontinent |
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