The detrital zircon U-Pb-Hf isotopes of the Triassic sediments in northern Pakistan: Implications for crustal evolution of the NW Indian continent

Lutfi, Wasiq; Sheikh, Lawangin; Zhao, Zhidan; Song, Shuguang; Qasim, Muhammad; Rahim, Yasin; Liu, Dong; Wang, Qing; Zhu, Di‐Cheng; Zhang, Liangliang; Tong, Xin; Lei, Hangshan; Awais, Muhammad

doi:10.1016/j.precamres.2021.106146

Cited by 5 publications

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“…In the last two decades, the detrital zircon U–Pb geochronology has been widely applied in sedimentary provenance interpretation (Baral et al, 2019; Chen et al, 2020; DeCelles et al, 2004; DeCelles, Gehrels, Quade, LaReau, & Spurlin, 2000; Ding et al, 2016; Gehrels et al, 2011; Lutfi et al, 2021; Najman, 2006; Najman, Carter, Oliver, & Garzanti, 2005). Similarly, the trace and rare‐earth elements' (REE) geochemistry is also important in reconstructing the provenance (Armstrong‐Altrin et al, 2015; Han, Zhang, Huang, Rui, & Tang, 2020; Nagarajan, Armstrong‐Altrin, Kessler, & Jong, 2017; Ramirez‐Montoya, Madhavaraju, & Monreal, 2021).…”

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confidence: 99%

Integrated provenance and tectonic implications of the Cretaceous–Palaeocene clastic sequence, Changla Gali, Lesser Himalaya, Pakistan

et al. 2021

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This study documented the field relationship and integrated provenance of a clastic sequence exposed at the Mesozoic–Cenozoic boundary located in Changla Gali section, Lesser Himalaya, Pakistan, to provide an insight into Cretaceous tectonics of the northern Indian margin. This boundary sequence is represented by the Early Palaeocene Hangu Formation, which consists of shales in the lower part and sandstone in the upper part. The contact relationship of the Early Palaeocene Hangu Formation with the underlying Late Cretaceous Kawagarh Formation is marked by an angular unconformity. The detrital zircons extracted from the shale and sandstone samples shows a major age cluster, which varies between ~700 and ~1,100 Ma (45%), ~1,600 and ~1,900 Ma (15%), and ~480 and ~590 Ma. Additionally, two minor age clusters of the detrital zircons are identified, that is, ~2,300–2,500 Ma and ~600–700 Ma. The younger detrital zircon grains have ages of 298 ± 4 Ma, 297 ± 4 Ma and 116 ± 3 Ma. This age pattern reflect the major source area as the Indian Plate. The two younger Permian zircon grains may be derived from the Panjal mafic volcanic rocks exposed in the vicinity of the study area. However, a single Cretaceous grain may be attributed to ophiolites, as well as Tethyan Himalayan (TH) volcanic rocks. Similarly, the sandstone petrographic results show that the sandstones are quartz‐rich, which show derivation from the craton interior provenance, which is likely the Indian Plate. However, the trace element data suggest a mixed source consisting of felsic and mafic rocks. The contribution of the mafic source is likely associated with the Panjal mafic rocks exposed along the northern Indian margin. The field relationship shows that the underlying Mesozoic sequence is folded prior to the deposition of the Hangu Formation. This folding suggests that the northern Indian margin experienced a regional compression during the Late Cretaceous time, which folded the Mesozoic sequence before the resumption of sedimentation during the Palaeocene. Furthermore, the detrital zircon provenance suggests that the sediments were mainly derived from the Indian Plate. Combining the results, it can be concluded that the compressional event is likely associated with the Late Cretaceous ophiolite obduction onto the leading edge of the Indian Plate. However, the absence of the major ophiolitic age component in the detrital record may suggest that the ophiolites were emplaced over the northern Indian margin but remained submerged during Early Palaeocene time.

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