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Research Projects
Fundamental Geosciences: Projects at District to
Regional Scales
Mark Barton and Eric Seedorff, Principal
Investigators
Two projects are proposed at the district to regional scales, both
in the Basin and Range project and with overlapping but distinct
sets of goals. They address several over-arching challenges: (1)
developing insights into how to more effectively explore at depth
and under post-mineral cover. The latter lands comprises >2/3
of the surface area in these highly mineralized regions. (2) Improving
our ability to assess the potential for and general distribution
of mineralized systems, and the distribution of other anomalous
materials in a rapidly urbanizing region, application to exploration,
base-line studies, and land-use and public policy considerations.
Both projects revolve around 4-D (3 spatial + time)
characterization of mineralized terrains –including developing a new paradigm
for continental extension with a focus on the Basin and Range Province
and a synthesis that compares key parts of the Basin and Range Province
with other areas. These two projects continue and extend long-standing
research efforts that have had and continue to have major support
from both industry (Phelps Dodge/FMI, Asarco, Quadra, Homestake/Barrick,
Anglo American) and the Federal government (mainly NSF, USGS).
Project group 2A
4-D characterization
of Cu-mineralized terrains in Arizona (and comparison with
other areas in the western Andes).
The two topics to be
developed under this SFAz initiative, in the context of
these issues are: (1) a regional-scale test of our developing,
novel ("multiple
half-graben") model for crustal extension with implications for the distribution
of mineralized materials, and (2) a systematic analysis of the variability
in the mineral ("metallogenic") potential of rocks of
different ages in this region and its implications for undiscovered
deposits. Both themes are routinely considered, and often used,
in mineral exploration in this region and world-wide. In this case
SFAz funding will leverage the existing partial support and allow
expansion and more timely completion of these projects. This project
will also provide an improved framework for several of the deposit-to-district
scale projects outlined above.
The extension (structural geology) project will
expand work done by our group in the Ray-Superior-Globe area and
in the Santa Catalina-Rincon Mountains through tying these two terrains
together via a synthesis of the intervening geology. The approach
will be to compile, reinterpret, and selectively re-map areas between
the Santa Catalina Mtns and the Tortilla Mtns (near Ray). This work
will enable new structural reconstructions, a test of alternative
structural models for continental extension, a broader interpretation
of the distribution of the major mineralized centers at San Manuel-Kalamazoo
and Copper Creek, and a deeper understanding of the geologic and
geochemical framework for the environmentally and hydrologically
important riparian areas of the San Pedro and Gila River drainages.
We anticipate interesting novel results that may show the relative
importance of natural processes on the mass balance of sulfur, metals,
and other materials in Tertiary and Quaternary sedimentary rocks.
Finally, we will continue close cooperation with USGS, industry,
and other professionals working in this area.
Project group 2B
4-D reconstruction of
Tertiary extension and hydrothermal systems in northeastern
Nevada.
These projects stem from long-standing questions
about the Tertiary structural and metallogenic evolution
of the northern Great Basin, which hosts the Nevada gold
province and the world-class, but enigmatic "Carlin-type" gold
deposits. Porphyry Cu(-Mo-Au) and related deposits are also widespread
in the region and of considerable economic importance. This theme
is of direct interest to several sponsors including Newmont, Quadra,
and BCE and should entice involvement from other companies. The
topic also links directly with district-focused projects including
work in the Battle Mountain, Robinson, and Eureka districts.
The northern Basin and Range province poses similar
structural puzzles to the southern Basin and Range (e.g., Arizona),
but has distinct differences in mineralization and rock types. Seedorff
and Barton have been involved in Great Basin geology for many years
and are proponents of alternative geologic models for Carlin-type
deposits as well as different structural interpretations (e.g., see
Cline et al., 2005, review of Carlin-type mineralization, 100th Ann.
Vol. of Economic Geology). We will build on a project begun by Dr.
Seedorff focused on the timing, reconstruction, and relationship
to mineral deposits in the greater Ruby Mountain area of NE Nevada.
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