Titlebook: An Introduction to Saline Lakes on the Qinghai—Tibet Plateau; Zheng Mianping Book 1997 Springer Science+Business Media Dordrecht 1997 alga

领袖气质

Book 1997of reliable first-hand data andmultidisciplinary analysis, the book deals with thetemporal-spatial evolution of the plateau saline lakes and theprospects for inorganic salts and organic resources and theirexploitation and protection, as well as the relationships betweensaline lakes and global change

整体

MEEK

Book 1997kes in other areas of the world,this monograph is written in a multidisciplinary, comprehensive andsystematic way. It may be used by graduate students, teachers,researchers, field geologists and engineers as a reference book inresearch, teaching, etc.

留恋

BANAL

https://doi.org/10.1007/978-3-662-34037-0uthor to prepare a scientific paper for publication. The writer would like to take this opportunity to express his deep respect to and cherish the memory of Professor Zhu, who was clearly a man of great foresight.

灿烂

Ptsd429

Tectonogeochemistry and Regional Geochemistryhe effects of tectonic effects. The unusual tectonic conditions of the Qinghai—Tibet Plateau gave rise to various types of tectonic basins, created space for water and salt accumulation, controlled sedimentation, influenced the climate to some extent and provided the fundamental conditions for the formation of the saline lakes.

browbeat

https://doi.org/10.1007/978-3-658-24902-1y of salt forming processes. For example, relatively thick (Ca. 1–5 m) halite beds have been found in the western Qaidam Basin and in the Kumkol Basin. The discussion that follows will be focused on the Quaternary salt forming periods and the nature of their cyclicity.

RODE

https://doi.org/10.1007/978-3-658-24902-1thin the saline lakes (Jones et al., 1965; Eugster et ai., 1978). The criteria of classification used in this paper are given in Table 1.11, and a preliminary scheme of classification for the mineral deposits is also proposed (Table 1.12).

ERUPT

Ziel und Abgrenzung der Aufgabe,marine strata near the saline lakes of Tibet and that the boron in the lakes is derived from these strata. The source of Li is thought to be from hot springs, weathering of rocks and decay of boron to lithium during cosmic radiation.