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Detrital zircon U-Pb age perspective on the sediment provenance and its geological significance of sandstones in the Lamandau region, SW Borneo, Indonesia

  • Geology
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Abstract

The Southwest Borneo (SW Borneo) block belongs to Sundaland and is the oldest continental fragment of Borneo that is believed to derive from the Gondwana land. The U-Pb isotopic dating ages of 113 detrital zircons from sandstones of the Ketapang Complex in SW Borneo range from 3 298 Ma to 78 Ma, and show six major age populations: 2 476–2 344 Ma, 2 016–1 831 Ma, 1 296–759 Ma, 455–406 Ma, 262–210 Ma, and 187–78 Ma. The youngest age of these detrital zircons is 78 Ma, indicating that the maximum depositional age of the sandstones is Campanian. Permian-Late Cretaceous detrital zircons are interpreted as having been derived from the nearby Schwaner Mountains and the Permian-Triassic tin belt granitoids in Southeast Asia (SE Asia). Archean-Carboniferous detrital zircons have a continental Gondwana provenance, with their age spectra similar to those of northwestern Australia, indicating that these zircons could be derived from the orogenic belts and cratons in northwestern and central Australia. The provenance of these detrital zircons in this study indicates the SW Borneo block was located on the northwestern margin of Australia during the Paleozoic, in the region of the Banda Embayment. SW Borneo rifted from Australia and moved northward in the Early Jurassic, and this block was added to Sundaland in the Early Cretaceous. The Luconia-Dangerous Grounds continental fragment derived from East Asia collided with SW Borneo after subduction in the Cretaceous, which induced the widespread magmatism in the Schwaner Mountains in SW Borneo.

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Data Availability Statement

The data that support the findings of this study are available from the corresponding author upon reasonable request.

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Acknowledgment

We thank Robert HALL (Department of Earth Sciences, SE Asia Research Group, Royal Holloway University of London, Egham, United Kingdom), the anonymous reviewers, and the editors for their helpful comments and suggestions.

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Authors and Affiliations

  1. Guangxi Key Laboratory of Hidden Metallic Ore Deposits Exploration, College of Earth Sciences, Guilin University of Technology, Guilin, 541004, China

    Shuang Li

  2. Center of Deep Sea Research, Institute of Oceanology, Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao, 266071, China

    Saijun Sun & Weidong Sun

  3. Laboratory for Marine Geology, Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao, 266237, China

    Saijun Sun & Weidong Sun

  4. CAS Key Laboratory of Crust-Mantle Materials and Environments, School of Earth and Space Sciences, University of Science and Technology of China, Hefei, 230026, China

    Xiaoyong Yang

  5. China Coal Geology Group Limited, Beijing, 100040, China

    Zhaojian Wu

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Correspondence to Saijun Sun.

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Supported by the National Natural Science Foundation of China (Nos. 41803038, 41903005), the Guangxi Natural Science Foundation (No. 2018GXNSFAA138193), and the China Postdoctoral Science Foundation (No. 2019M662458)

Electronic supplementary material

343_2021_405_MOESM1_ESM.xls

Table 1S LA-ICP-MS U-Pb zircon analytical results for sandstones of the Ketapang complex in the Lamandau region, SW Borneo, Indonesia

343_2021_405_MOESM2_ESM.xls

Table 2S REE and trace elements (ppm) results of zircons from sandstones of the Ketapang complex in the Lamandau region, SW Borneo, Indonesia

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Li, S., Sun, S., Yang, X. et al. Detrital zircon U-Pb age perspective on the sediment provenance and its geological significance of sandstones in the Lamandau region, SW Borneo, Indonesia. J. Ocean. Limnol. 40, 496–514 (2022). https://doi.org/10.1007/s00343-021-0405-6

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