G. Einsele et al.
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Evolution and Facies Architecture of A Himalayan Cretaceous Forearc Basin G. Einsele et al.
Berita Sedimentologi Vol 7, No 1 (1998)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (782.892 KB) | DOI: 10.51835/bsed.1998.7.1.289

Abstract

The mid-Cretaceous to Eocene flysch deposits of the Xigaze forearc basin in southern Tibet were investigated in a 120 km segment along the Indus Yarlung suture zone. The basin evolved south of the magnetic arc (Gangdise belt) of the Lhasa block on top of trapped oceanic or transitional crust.