Metallogeny of the Altaids
– Identifying new terranes BASED ON
INTERDISCIPLINARY
GEOTRAVERSE STUDY
Seltmann R. & CERCAMS team*, Borisenko A.S. & SB RAS team**,
Petrov O., Shatov V., Shevchenko S., Sergeev S.***
*Centre for Russian and
Central EurAsian Mineral Studies, NHM, London, UK, rs@nhm.ac.uk
**Institute
for Geology and Mineralogy SB RAS, Novosibirsk, Russia,
borisenko@uiggm.nsc.ru
***
VSEGEI, St Petersburg, Russia, vsgdir@vsegei.ru
The Altaid orogenic collage
extends from the Urals over Central Asia (Kazakhstan, Tien Shan) to
the Mongol-Okhotsk belt. It comprises assembled fragments of
sedimentary basins, island arcs, accretionary wedges and
microcontinents of Neoproterozoic to Cenozoic age now joined to
surrounding continental regions (e.g. East European craton). The
clockwise rotation of Siberia relative to Eastern Europe during
middle and late Paleozoic resulted in multiple episodes of arc
collisions, both between themselves and with the cratons, as well as
the progressive oroclinal bending. This complex cycle of rifting,
subduction, accretion and collision has culminated in the current
complex assembly.
Despite the wealth of documented
deposit types of undoubted high economic value and the wealth of
empirical information and genetic interpretations concerning the
individual deposits, inter-terrane correlation in the region is
sketchy at best. This is a legacy of the past political and physical
barriers against compilation work in a huge area of enormous
geological complexity.
Based on
utilization of existing data a working model of paleogeographic
reconstruction and tectonic modelling has been assembled. Selective
mapping in specific terranes has been used by to improve the existing
database coupled with targeted wholerock geochemistry and precise
geochronology. Proterozoic crustal slivers and Paleozoic
oceanic-subduction-accretion complexes with former magmatic arcs in
the regions formed the first priorities for established correlation.
These could be better defined in time and space using new data,
reconstructing their current and past distribution patterns, defining
regionally controlling major fault structures and post-depositional
processes. From this, known terranes hosting key deposit types were
extrapolated into geographical gaps in exploration activity and new
prospective regions could be outlined.
Based on the precursor study of
the CERCAMS team and associated partners in the Eastern and Western
Altaids situated to the south of Russian state border, and based on
the vast experience and data sets existing in the research
institutions of Russia, the three research teams have agreed to
combine their efforts in a follow-up approach extending the study
into Russian territory to the south of the Siberian craton from the
Altai Republic in the west to Chita and Amur regions in the east.
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