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all geography including DSDP/ODP Sites and Legs
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sedimentary structures
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sedimentary structures
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graphite deposits
Large-scale 3D inversion of semi-airborne electromagnetic data — Topography and induced polarization effects in a graphite exploration scenario
MINING PENCILS, SCULPTING GRAPHITE: THE SIBERIAN EXPEDITION OF J.-P. ALIBERT (1844–1857) AND THE EVOLVING 19TH CENTURY EUROPEAN VISUAL AND MATERIAL CULTURE RELATED TO EARTH SCIENCES
Petrology of the Kureika Graphite Deposit in the Roof of the First-Rapid Trap Intrusion (Siberian Platform)
The need for joined-up thinking in critical raw materials research
Affinity and Petrogenesis of the Huzyk Creek Metal-Enriched Graphite Deposit: A Metamorphosed Metalliferous Black Shale in the Trans-Hudson Orogen Of Manitoba, Canada
Geochemical characteristics and indication of graphite deposits in Xinrong Region, Shanxi, China
Graphite paradox in Baikal geyserite paleovalley, Russia
Graphite from Palaeoproterozoic enhanced carbon burial, and its metallogenic legacy
Self-potential Data Interpretation for Two Co-axial Structures Utilizing the RMS Parameter
Effects of full transmitting-current waveforms on transient electromagnetics: Insights from modeling the Albany graphite deposit
The Vanadium-bearing Oxide Minerals of the Green Giant Vanadium-graphite Deposit, Southwest Madagascar
Abstract An integrated interpretation of the east Kimberley, northern Western Australia was completed to determine mineral prospectivity, and was centred on a portion of a magnetotelluric (MT) survey conducted across the entire Kimberley Craton and surrounding orogens. A structural geophysical interpretation used potential field data, and was constrained by geological field observations, petrophysics, remote sensing and understanding of the tectonic history of the region. Potential field forward modelling located along the same survey traverse as the MT data allowed comparison between the two datasets and their interpretations revealing interesting features suggesting the presence of large-scale structures, the presence of mineralization deep in the crust, and where mineralization may be at or near the surface. The King River Fault is shown from both the MT inversion and potential field modelling as a crustal-scale, west-dipping structure, the footwall of which bounds the western side of a large resistive body. A conductive anomaly is also located on the hanging wall of the King River Fault. Our assessment suggests that graphitic rocks, most likely with some sulphide content, contribute to the strength of this anomaly, and highlights the potential of the east Kimberley to host graphite and base metal deposits.