A NEW MECHANISM OF SYNGENETIC SEDIMENTARY ENRICHMENT OF ORE MATERIALS:MIXING OF MOVING SEA-WATER MASSES
Received date: 1993-06-14
Online published: 1994-03-01
Just as in the atmosphere, the moving and interacting of gas masses results in various climatatic and meteorological phenomena,there are also in oceans many sea-water masses. Whose movement and interaction results in various oceanic phenomena. Mixing occuring on the oceanic frontal zones between water masses can lead to syngenetic sedimentary enrichment of ore-building materials. This is a new mechanism of ore-building for sedimentary deposits and for source beds in sedimentary rocks. It occurs very often on the earth surface through the geological time, but is not yet well known.
Liu Jianming . A NEW MECHANISM OF SYNGENETIC SEDIMENTARY ENRICHMENT OF ORE MATERIALS:MIXING OF MOVING SEA-WATER MASSES[J]. Advances in Earth Science, 1994 , 9(2) : 24 -28 . DOI: 10.11867/j.issn.1001-8166.1994.02.0024
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