syngenetic


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syn·ge·net·ic

(sin'jĕ-net'ik),
Relating to syngenesis.

syn·ge·net·ic

(sin'jĕ-net'ik)
Relating to syngenesis.
References in periodicals archive ?
Most likely, the finer glauconite fraction, which was subjected to XRD analyses, reflects syngenetic conditions while the coarser one represents rather a redeposition history.
To be accepted as bona fide, ancient microfossils must be structurally preserved biogenic remnants that are indigenous to and syngenetic with the primary deposition of sedimentary rocks of known stratigraphic and geographic source and established age (5, 14).
It is a large, syngenetic magma body composed of basic and ultra-basic rocks emplaced an estimated 2.
Initial results have been encouraging in that certain trace elements may assist in the identification of specific schist units associated with syngenetic gold mineralization.
This occurrence is a stratabound pod and was originally interpreted as a syngenetic VMS showing (e.
When exploitation in altered oecotopes corresponding to this type of forest is excluded, a syngenetic evolution by enrichment and competition among species is also developed, up to reach a stage of secondary tree shrubwood, in which few species dominate the coverage.
41, 12, 20], or 2) flushing of the sediments by metal-enriched syngenetic brines or contemporaneous exhalation of such brines into marine basin, e.
The U occurrences are syngenetic and appear to bear some similarities to the world-class Uranium deposit of Rossing in Namibia (Laznicka 1993), which is characterized by low-grade ore (approx.
All of the topaz thus far recovered has been found in miarolitic, syngenetic pegmatites in the Mesozoic alkali granite (Menzies, 1995).
Syngenetic barite and subordinate amounts of low-grade sulphide rock and silica rock were deposited as sediments.
In the Precordillera and Frontal Cordillera areas (San Juan and Mendoza provinces), syngenetic mineral deposits are associated with ophiolites in suture zones that carry chromite, magnetite and massive sulphides, talc and asbestos; the talc and asbestos have resulted from post-ophiolite metamorphism.
According to Argold in 1992, "The occurrences appear to be of syngenetic organic origin and can therefore be expected to occupy a specific stratigraphic facies within the Masterton, and show lateral continuity [within EL22251 at Selby].