Integrated litho-ichnofacies and ichnofabric analysis of the lowermost part of the Kunzum La Formation along the Khemangar khad and the Parahio Valley sections, Spiti Region (Zanskar-Spiti-Kinnaur Basin), Northwest Himalaya, India

• Published in: Journal of the Geological Society of India Vol. 85; no. 5; pp. 557 - 566
• Main Authors: Virmani, Nancy, Singh, Birendra P., Gill, Aman
• Format: Journal Article
• Language: English
• Published: New Delhi Springer India 01.05.2015; Springer Nature B.V
• Subjects: Banks; Cambrian; Deposition; Earth and Environmental Science; Earth Sciences; Exposure; Formations; Geology; Hydrogeology; Lithosphere; Marine; Marine environment; Rocks; Shallow water; Strata; Stratification; Stratigraphy; Valleys; India; Pakistan, Himalayas; India, Himalaya, Parahio Valley, Spiti Region; Litho-ichnofacies; ichnofabric analysis; archetypal; facies; wave-dominated shallow water environment; Formation; Kunzum
• ISSN: 0016-7622; 0974-6889
• DOI: 10.1007/s12594-015-0250-3

The Cambrian sequence, designated as the Kunzam La Formation, is exposed along the c La ssical Parahio Valley section and also on left bank of the Khemangar khad in the Parahio Valley (Spiti), the La tter constitutes the lowermost exposed part of the Kunzum La Formation. The lower part of the Parahio Valley section and outcrop near the left bank of the Khemangar khad were studied for integrated litho-ichnofacies and ichnofabric analysis. The study establishes a genetic re La tionship of the strata of these two localities. Five lithofacies are recognised in both the examined sections. The lithofacies indicate a wave-dominated shallow marine environment of deposition for these Cambrian rocks. The overall calcu La ted ichnofabric indices in 74 m exposed strata at the Khemangar khad locality range from ii1= 80 .% (represented by 25.8 m), ii 2 = 17 % (represented by 5.4 m) and ii 4 = 2.5 % (represented by 0.8 m). The 42 m rocks examined in the main Parahio Valley section indicate ichnofabric indices ranging from ii 1 = 37 % (represented by 17.8 m), ii 2 = 21 % (represented by 8.0 m), ii 3 = 40 % (represented by 15.2 m) and ii 4 = 2.0 % (represented by 1.0 m). The presence of archetypal Cruziana ichnofacies, parallel and wavy La minations, hummocky cross stratification (HCS) and trough cross stratification (TCS) supports a wave-dominated shallow water environment from upper shoreface to middlelower shoreface setup for the deposition of the lowermost part of the Kunzum La Formation in the Parahio Valley.