Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

Modern nonmarine evaporite deposition, Quaidam basin, China: An overview

Conference · · AAPG Bulletin (American Association of Petroleum Geologists); (United States)
OSTI ID:7013226
; ;  [1];  [2];  [3]
  1. SUNY Binghamton, NY (United States)
  2. Univ. of Calgary, Alberta (Canada)
  3. Inst. of Salt Lakes, Xining (China)

Dabusun Lake (200 km{sup 2}) is a shallow ({lt}1 m) perennial saline lake in the high altitude Qaidam basin (120,000 km{sup 2}) of western China. It is underlain by {gt}40 m of salt and siliciclastic sediments ({approximately}54,000 years old). Petrographic features in two 50 m cores (chevron halite, halite cumulates, rafts, and siliciclastic mud, minor solution and no subaerial exposure features except in the top meter) indicate continuous shallow perennial lake conditions. The chemical composition of fluid inclusions trapped in halite crystals show lakewaters have generally undergone progressive concentration to the present. Modern Dabusun Lake is chemically uniform (Na-Mg-Cl-rich), nonstratified, and at or near halite saturation. Evaporites accumulate in zones on the restricted lake margins as halite (cumulate and raft layers with rippled surfaces and chevron mounds), halite + carnallite (KCl{center dot}MgCl{sub 2}{center dot}6H{sub 2}O), and finally carnallite (ephemeral fine-grained crystal mush). The carnallite zone merges with a 25 m wide shoreline facies, highlighted by a 1 m wide zone of halite ooids/pisoids that border a 20-30 cm tall overhanging salt crust (1967 shoreline). Lower lake levels since that time have produced vadose diagenetic features in the shoreline halites including: pendant cements, meniscus cements, halite 'popcorn,' and solution voids with muddy geopetal fills. A large flood (July-September 1989) expanded Dabusun Lake to 800 km{sup 2}, and dissolved all surface carnallite deposits. Diagenetic carnallite cements, formed by downward migration and cooking of carnallite saturated surface brines, however, remain in the subsurface to depths of 13 m. These potash mineral cements are similar in texture to many ancient potash evaporites.

OSTI ID:
7013226
Report Number(s):
CONF-910403--
Journal Information:
AAPG Bulletin (American Association of Petroleum Geologists); (United States), Journal Name: AAPG Bulletin (American Association of Petroleum Geologists); (United States) Vol. 75:3; ISSN AABUD; ISSN 0149-1423
Country of Publication:
United States
Language:
English

Similar Records

Evaporite deposition in a shallow perennial lake, Qaidam basin, western China
Conference · Thu Feb 28 23:00:00 EST 1991 · AAPG Bulletin (American Association of Petroleum Geologists); (United States) · OSTI ID:7259424

Halite depositional facies in a solar salt pond: A key to interpreting physical energy and water depth in ancient deposits
Journal Article · Wed Aug 01 00:00:00 EDT 1990 · Geology; (USA) · OSTI ID:6313708

Petrographic and geochemical constraints on the deposition and diagenesis of the Haynesville Formation (Upper Jurassic), southwestern Alabama
Conference · Thu Feb 28 23:00:00 EST 1991 · AAPG Bulletin (American Association of Petroleum Geologists); (United States) · OSTI ID:5739776