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Provenance of detrital zircons in the Late Triassic Sichuan foreland basin: constraints on the evolution of the Qinling Orogen and Longmen Shan thrust-fold belt in central China

Yong ZhangState Key Laboratory for Mineral Deposits Research, Institute of Energy Sciences and Department of Earth Sciences, Nanjing University, Nanjing, ChinaView further author information

Dong JiaState Key Laboratory for Mineral Deposits Research, Institute of Energy Sciences and Department of Earth Sciences, Nanjing University, Nanjing, ChinaCorrespondence[email protected]
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Li ShenState Key Laboratory for Mineral Deposits Research, Institute of Energy Sciences and Department of Earth Sciences, Nanjing University, Nanjing, ChinaView further author information

Hongwei YinState Key Laboratory for Mineral Deposits Research, Institute of Energy Sciences and Department of Earth Sciences, Nanjing University, Nanjing, ChinaView further author information

Zhuxin ChenResearch Institute of Petroleum Exploration & Development, PetroChina, Beijing, ChinaView further author information

Haibin LiState Key Laboratory for Mineral Deposits Research, Institute of Energy Sciences and Department of Earth Sciences, Nanjing University, Nanjing, ChinaView further author information

Zhigang LiState Key Laboratory for Mineral Deposits Research, Institute of Energy Sciences and Department of Earth Sciences, Nanjing University, Nanjing, ChinaView further author information

Chuang SunState Key Laboratory for Mineral Deposits Research, Institute of Energy Sciences and Department of Earth Sciences, Nanjing University, Nanjing, ChinaView further author information

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Supplemental material

Figure S2. Published age spectra of detrital zircons from the Late Triassic Sichuan foreland basin.

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Figure S1. U-Pb Concordia plots for zircons from our sandstone samples.

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Table S2. LA-MC-ICPMS zircon Lu-Hf isotopic data for the Upper Triassic sandstone in the Sichuan foreland basin, NW South China Block.

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Table S1. LA-ICP-MS zircon U-Pb isotopic data for the sandstones in the Sichuan foreland basin, NW South China Block.

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Provenance of detrital zircons in the Late Triassic Sichuan foreland basin: constraints on the evolution of the Qinling Orogen and Longmen Shan thrust-fold belt in central China

Figure S2. Published age spectra of detrital zircons from the Late Triassic Sichuan foreland basin.

Figure S1. U-Pb Concordia plots for zircons from our sandstone samples.

Table S2. LA-MC-ICPMS zircon Lu-Hf isotopic data for the Upper Triassic sandstone in the Sichuan foreland basin, NW South China Block.

Table S1. LA-ICP-MS zircon U-Pb isotopic data for the sandstones in the Sichuan foreland basin, NW South China Block.

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Provenance of detrital zircons in the Late Triassic Sichuan foreland basin: constraints on the evolution of the Qinling Orogen and Longmen Shan thrust-fold belt in central China

Figure S2. Published age spectra of detrital zircons from the Late Triassic Sichuan foreland basin.

Figure S1. U-Pb Concordia plots for zircons from our sandstone samples.

Table S2. LA-MC-ICPMS zircon Lu-Hf isotopic data for the Upper Triassic sandstone in the Sichuan foreland basin, NW South China Block.

Table S1. LA-ICP-MS zircon U-Pb isotopic data for the sandstones in the Sichuan foreland basin, NW South China Block.

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