Dabiele's position at the south end of the playa means that its waters are relatively less influenced by the concentrated
mineral springs along the playa's northern boundary. As with
Xiaobiele, it is nonetheless nearly saturated with
calcite,
anhydrite,
halite, and (importantly)
carnallite, which is processed to produce
potash for
potassium-rich
fertilizers and other uses. The Bieletan subbasin as a wholeinclusive of
Suli,
S. Suli, and
Xiaobieleis also the richest source of
brine lithium in China, with an estimated store of of
lithium chloride. The lithium derives from
hot springs located near
Mount Buka Daban which now feed the
Narin Gol River or
Hongshui River Hóngshuǐ Hé) that flows into
East Taijinar Lake. In the past, however, the springs lay within the "Kunlun"
paleolake which until about 30,000 years ago produced a river which flowed north into a broad
alluvial fan feeding the
"Qarhan" paleolake in the
Sanhu area. Bieletan's lithium came both from deposits directly flowing into the area at the time and continuing contributions from the
Urt Moron and other rivers arising in and flowing through the former alluvial plain. ==See also==