Pv. Koval et al., Database of granites in the Mongol-Okhotsk zone, Mongolia-Siberia, and itsuse in mineral exploration, J GEOCHEM E, 66(1-2), 1999, pp. 199-210
The Mongol-Okhotsk zone (MOZ) forms an arcuate belt up to 1000 km wide stre
tching over 3000 km eastwards from Central Mongolia to the Sea of Okhotsk.
The extensive suite of granitoids and related mineralization were formed du
ring the Mesozoic. The results of analysis of geochemical data from the MOZ
, which are currently managed at the Institute of Geochemistry in Irkutsk (
IGC), are presented in the form of a geochemical data model. The available
data were obtained during the past 30 years and include coverage of more th
an 900 granite massifs, and data are still being accumulated. The relationa
l database is a model providing access to multiple data files via common fi
elds using the PARADOX 5.0 database management systems. An entity relations
hip diagram technology was used for constructing the database model. The da
tabase makes it possible to provide a generalization and analysis of geoche
mical data related to metallogeny on new informational levels based on the
concept of the ore-bearing potential of granitoid types and the ore product
ivity of intrusions. A general hierarchical metallogenic scheme has been de
veloped. (C) 1999 Elsevier Science B.V. All rights reserved.