Thermobaric structure of the Himalayan Metamorphic Belt in Kaghan Valley, Pakistan

• Published in: Journal of Asian earth sciences 2007-02, Vol.29 (2), p.390-406
• Main Authors: Rehman, Hafiz Ur, Yamamoto, Hiroshi, Kaneko, Yoshiyuki, Kausar, Allah Bakhsh, Murata, Mamoru, Ozawa, Hiroaki
• Format: Article
• Language: English
• Subjects: Coesite-bearing eclogites; Kaghan Valley; P–T conditions; Thermobaric structure
• ISSN: 1367-9120; 1878-5786
• DOI: 10.1016/j.jseaes.2006.06.002

The thermobaric structure of the Himalayan Metamorphic Belt (HMB) has been constructed along the Kaghan Valley transect, Pakistan. The HMB in this valley represents mainly the Lesser Himalayan Sequence (LHS) and Higher Himalayan Crystallines (HHC). Mineral parageneses of 474 samples, from an approximately, 80-km traverse from southwest to northeast, were examined. Microprobe analyses were carried out to quantify the mineral composition. To determine the pressure–temperature (P–T) conditions, 65 thin sections (7 pelites from LHS and 25 pelites, 9 mafic rocks/amphibolites and 19 eclogites from HHC) were selected. Based on field observations and mineral paragenesis, low-grade to high-grade metapelites, show Barrovian-type progressive metamorphic sequence, with chlorite, biotite, garnet and staurolite zones in LHS and staurolite, kyanite and sillimanite zones in HHC. By using well-calibrated geothermobarometers, P–T conditions for pelitic and mafic rocks are estimated. P–T estimates for pelitic rocks from the garnet zone indicate a condition of 534 ± 17 °C at 7.6 ± 1.2 kbar. P–T estimates for rocks from the staurolite and kyanite zones indicate average conditions of 526 ± 17 °C at 9.4 ± 1.2 kbar and 657 ± 54 °C at 10 ± 1.6 kbar, respectively. P–T conditions for mafic rocks (amphibolites) and eclogites from HHC are estimated as 645 ± 54 °C at 10.3 ± 2 kbar and 746 ± 59 °C at 15.5 ± 2.1 kbar, respectively. The coesite-bearing ultrahigh-pressure (UHP) eclogites record a peak P–T condition of 757–786 °C at 28.6 ± 0.4 kbar and retrograde P–T conditions of 825 ± 59 °C at 18.1 ± 1.7 kbar. These results suggest that HMB show a gradual increase in metamorphic grade from southwest to northeast. The P–T conditions from Pelitic and adjacent mafic rocks having identical peak conditions in the same metamorphic zone, while the structural middle in HHC reached the highest P–T condition upto the UHP grade.