Abstract
Phosphorus distributions are given for Central Aldan Mesozoic magmatites, mainly for the dike complex within the Seligdar apatite-carbonate ore deposit. The highest phosphate levels occur in the pyroxenites of the leucitite-syenite subassociation, but these rocks occur only on a restricted scale. The trachyte dikes have assimilated phosphorus from the surrounding apatite ores with the formation of an aureole of dike rocks anomalous in P2O5, including those in the upper structural level above the deposit. The assimilation is accompanied by calcitization in the dikes and by dedolomitization in the surrounding ores, where apatite calcite rocks are formed. -Journal summary
| Original language | English |
|---|---|
| Pages (from-to) | 41-49 |
| Number of pages | 9 |
| Journal | Geochemistry International |
| Volume | 25 |
| Issue number | 2 |
| Publication status | Published - 1988 |
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ASJC Scopus subject areas
- Geochemistry and Petrology
- Geophysics
Cite this
Phosphorus in Mesozoic intrusives in the region of the Seligdar apatite deposit. / Boyarko, G. Y.
In: Geochemistry International, Vol. 25, No. 2, 1988, p. 41-49.Research output: Contribution to journal › Article
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TY - JOUR
T1 - Phosphorus in Mesozoic intrusives in the region of the Seligdar apatite deposit
AU - Boyarko, G. Y.
PY - 1988
Y1 - 1988
N2 - Phosphorus distributions are given for Central Aldan Mesozoic magmatites, mainly for the dike complex within the Seligdar apatite-carbonate ore deposit. The highest phosphate levels occur in the pyroxenites of the leucitite-syenite subassociation, but these rocks occur only on a restricted scale. The trachyte dikes have assimilated phosphorus from the surrounding apatite ores with the formation of an aureole of dike rocks anomalous in P2O5, including those in the upper structural level above the deposit. The assimilation is accompanied by calcitization in the dikes and by dedolomitization in the surrounding ores, where apatite calcite rocks are formed. -Journal summary
AB - Phosphorus distributions are given for Central Aldan Mesozoic magmatites, mainly for the dike complex within the Seligdar apatite-carbonate ore deposit. The highest phosphate levels occur in the pyroxenites of the leucitite-syenite subassociation, but these rocks occur only on a restricted scale. The trachyte dikes have assimilated phosphorus from the surrounding apatite ores with the formation of an aureole of dike rocks anomalous in P2O5, including those in the upper structural level above the deposit. The assimilation is accompanied by calcitization in the dikes and by dedolomitization in the surrounding ores, where apatite calcite rocks are formed. -Journal summary
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UR - http://www.scopus.com/inward/citedby.url?scp=0024225923&partnerID=8YFLogxK
M3 - Article
AN - SCOPUS:0024225923
VL - 25
SP - 41
EP - 49
JO - Geochemistry International
JF - Geochemistry International
SN - 0016-7029
IS - 2
ER -