2021
DOI: 10.1016/j.earscirev.2021.103789
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Detrital zircon U Pb age distributions and Hf isotopic constraints of the Ailaoshan-Song Ma Suture Zone and their paleogeographic implications for the Eastern Paleo-Tethys evolution

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Cited by 23 publications
(48 citation statements)
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“…In southwestern China and northern Vietnam, the Indosinian Orogeny between the SCB and IB consists of three tectonic belts separated by the Red River fault (RRF) and Dien Bien Fu fault (DBF, Fig. 1), namely the Song Ma belt in SE, and the Song Chay belt in NE, and the Ailaoshan belt in NW (Lepvrier et al, 2008(Lepvrier et al, , 2011Faure et al, 2014Faure et al, , 2016aLi et al, 2021).…”
Section: Geological Settingmentioning
confidence: 99%
See 1 more Smart Citation
“…In southwestern China and northern Vietnam, the Indosinian Orogeny between the SCB and IB consists of three tectonic belts separated by the Red River fault (RRF) and Dien Bien Fu fault (DBF, Fig. 1), namely the Song Ma belt in SE, and the Song Chay belt in NE, and the Ailaoshan belt in NW (Lepvrier et al, 2008(Lepvrier et al, , 2011Faure et al, 2014Faure et al, , 2016aLi et al, 2021).…”
Section: Geological Settingmentioning
confidence: 99%
“…The plutons have low 87 Sr/ 86 Sr(i) and δ 18 O values with high-Mg # values and are I-type with positive ε Nd (t) and ε Hf (t) values (Qian et al, 2019).at the plutons developed in a continental-arc setting (Kamvong et al, 2014;Hoa et al, 2008). Therefore, the Truong Son-Sam Nua zone represents the magmatic arc related to the southwestward subduction of the Paleo-Tethys Ocean (e.g., Liu et al, 2012;Hieu et al, 2016;Wang et al, 2016Wang et al, , 2018Hou et al, 2019;Qian et al, 2019;Li et al, 2021).…”
Section: Song Ma Beltmentioning
confidence: 99%
“…The sedimentary archives of the foreland basins are extensively analyzed using modern techniques such as U-Pb dating [4][5][6][7][8] to estimate the maximum depositional ages and constrain the sediment provenance. This is a powerful tool in identifying the precise information about the sediment provenance, which is very important in explaining the paleogeographic reconstructions of the terranes in geological history [9][10][11]. Furthermore, this technique has also been widely applied in constraining the timing of orogenic events such as Ophiolite obduction and final collision in the Himalayan orogen [4,10].…”
Section: Introductionmentioning
confidence: 99%
“…This is a powerful tool in identifying the precise information about the sediment provenance, which is very important in explaining the paleogeographic reconstructions of the terranes in geological history [9][10][11]. Furthermore, this technique has also been widely applied in constraining the timing of orogenic events such as Ophiolite obduction and final collision in the Himalayan orogen [4,10]. The Himalayan foreland basin attained significant attraction in the last three decades to address the timing and location of the initial India-Asia collision using the foreland basing sedimentary archives [1,6,7,[12][13][14][15][16].…”
Section: Introductionmentioning
confidence: 99%
“…Magmatic rocks are poorly exposed along the Paleo-Tethyan Ocean between the South China Craton and Indochina Block (Figure 1), and thus its subduction polarity has been controversial. Some studies suggested that the subduction was bidirectional (e.g., Zhong et al, 2013;Hou et al, 2017;Xia et al, 2019;Xu et al, 2019), whereas other studies argued that the subduction was unidirectional (e.g., Faure et al, 2014;Ngo et al, 2016;Yu et al, 2016;Gan et al, 2021;Li et al, 2021;Wang et al, 2021). The latter suggested that the southwestern margin of the South China Craton was a passive continental margin (Yan et al, 2019), and the Paleo-Tethyan Ocean may only undergo a subduction westward beneath the Indochina Block during the Late Permian-Early Triassic (Jian et al, 2009;Faure et al, 2014;Ngo et al, 2016;Li et al, 2021;Wang et al, 2021).…”
Section: Introductionmentioning
confidence: 99%