The Location of Qinling Orogenic Belt
- Details
- Category: Molybdenum knowledge
- Published on 07 August 2013
- Hits: 339
It can be easily oxidized to form water-soluble MoO4- in the surface environment, especially in the Phanaerozoic, and then precipitated under anoxic conditions.
Therefore, closed or semi-closed water bodies with large catchment areas and high chemical erosion rates are the most favourable locations for molybdenum-enriched sediments.
The Qinling orogenic belt was located in the tropics during crustal collisions, such that the chemical erosion was presumably intense.
Whereas the Erlangping back-arc basin was probably a closed or semi-closed water body as a result of plate convergence.
More molybdenum product: http://www.molybdenum.com.cn
Tel: 0592-5129696 Fax：0592-5129797
E-mail:
This email address is being protected from spambots. You need JavaScript enabled to view it.
Tungsten Picture Center: http://picture.chinatungsten.com
Tungsten Video Center: http://v.chinatungsten.com
Tungsten News & Tungsten Prices, 3G Version: http://3g.chinatungsten.com
sales@chinatungsten.com