Geochemical and geochronological evidence of meteorite impact excavating the Archean basement at Lonar Crater, Central India

• Published in: Lithos Vol. 404-405; p. 106479
• Main Authors: Chandran, Saranya R., James, S., Santosh, M., Yang, Cheng-Xue, Zhang, Cun, Rajesh, V.J., Satyanarayanan, M., Praveen, M.N., Anilkumar, Y., Singh, S.P., Keerthy, S., Sajinkumar, K.S.
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01-12-2021
• Subjects: Cristobalite; Impact melt-bearing rock; Lonar; Meteorite impact crater; Zircon U-Pb geochronology; Impact melt-bearing rock; Cristobalite; Zircon U-Pb geochronology; Meteorite impact crater; Lonar
• ISSN: 0024-4937; 1872-6143
• DOI: 10.1016/j.lithos.2021.106479

The effect of meteorite impact on basement rocks remains widely debated at Lonar Crater, Central India. We investigate an impact melt-bearing rock from the ejecta layer of Lonar to assess the potential interaction of the projectile with the underlying Archean basement. The investigated sample is a melanocratic, aphanitic melt rock comprising glassy inclusions, and plagioclase and quartz clasts. Plagioclase and quartz show shock-induced features including diaplectic glass and well-developed planar deformation features (PDFs), respectively. The decrease in shock pressure is thus established with the plagioclase of overlying basalt showing shock features like diaplectic glass whereas the quartz from lower Archean basement showing PDF development. Laser Raman spectroscopy reveals the presence of cristobalite. The impact melt-bearing rock shows major element geochemistry similar to that of Deccan basalt with a tholeiitic trend, but the Harker variation plots reveal an independent field for the melt rock between the two end members: Deccan basalt and Archean basement represented by Peninsular gneiss. The REE geochemistry also reveals more fractionation for the melt rock. Zircon U-Pb data indicate an upper intercept age around 3.0 to 3.1 Ga. Chondrite normalized zircon REE data display a positive Eu anomaly indicating a reheating during the impact event. This indicates that the melt rock sample was generated by the incorporation of Archean basement gneiss components, which is compatible with the estimated depth of excavation for an impact structure of this size. This specifies a depth to basement in the range between 522 and 570 m.
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•Tracking the involvement of Archean basement rocks during impact event.•Shock features in quartz grains including PDFs and mosaicism•Whole rock REE and zircon REE geochemistry reveals the contribution of basement rock.•Zircon U-Pb ages of 3.0 to 3.1 Ga provide robust evidence of basement rock as the source.