A sequence of paralic strata which contains biota fossils from Early-Middle Devonian is found in Bukadaban district in west-middle section of East Kunlun Mt. and it is certained there is the strata of Devonian period.

• 摘要在东昆仑中西段布喀达阪峰地区发现了一套含早－中泥盆世生物化石的海陆交互相地层，从而确定了该地区泥盆纪地层的存在。