Airborne hyperspectral imaging of hydrothermal alteration zones in granitoids of the Eastern Fold Belt, Mount Isa Inlier, Australia
暂无分享,去创建一个
Thomas Cudahy | Robert Hewson | Nicholas H.S. Oliver | Carsten Laukamp | James S. Cleverley | T. Cudahy | R. Hewson | N. Oliver | J. Cleverley | C. Laukamp
[1] S. Taylor,et al. Geochemistry of eocene calc-alkaline volcanic rocks from the Kastamonu area, Northern Turkey , 1976 .
[2] M. McCulloch,et al. Petrology, geochronology and isotope geochemistry of the post-1820 Ma granites of the Mount Isa Inlier: mechanisms for the generation of Proterozoic anorogenic granites , 1988 .
[3] Geordie Mark. Nd isotope and petrogenetic constraints for the origin of the Mount Angelay igneous complex: implications for the origin of intrusions in the Cloncurry district, NE Australia , 2001 .
[4] C. Fanning,et al. Age constraints on the tectonothermal evolution of the Selwyn Zone, Eastern Fold Belt, Mount Isa Inlier , 2008 .
[5] D. Blake. Geology of the Mount Isa Inlier and environs, Queensland and Northern Territory , 1987 .
[6] J. Austin,et al. The 1800-1610 Ma stratigraphic and magmatic history of the Eastern Succession, Mount Isa Inlier, and correlations with adjacent Paleoproterozoic terranes , 2008 .
[7] J. A. Grant. The isocon diagram; a simple solution to Gresens' equation for metasomatic alteration , 1986 .
[8] Geordie Mark,et al. Magmatic–hydrothermal albite–actinolite–apatite-rich rocks from the Cloncurry district, NW Queensland, Australia , 2000 .
[9] R. Clark,et al. High spectral resolution reflectance spectroscopy of minerals , 1990 .
[10] Shaun K. Frape,et al. Chlorine stable isotope ratios as tracer for pore‐water advection rates in a submarine gas‐hydrate field: implication for hydrate concentration , 2006 .
[11] Patrick J. Williams,et al. Giant metasomatic system formed during exhumation of mid‐crustal Proterozoic rocks in the vicinity of the Cloncurry Fault, northwest Queensland , 1995 .
[12] Geordie Mark,et al. Mineralogical and chemical evolution of the Ernest Henry Fe oxide–Cu–Au ore system, Cloncurry district, northwest Queensland, Australia , 2006 .
[13] T. Baker,et al. Modeling the Role of Sodic Alteration in the Genesis of Iron Oxide-Copper-Gold Deposits, Eastern Mount Isa Block, Australia , 2004 .
[14] Geordie Mark,et al. Geochemistry of post-1540 Ma granites in the Cloncurry District, Northwest Queensland , 1998 .
[15] Geordie Mark. Albitite formation by selective pervasive sodic alteration of tonalite plutons in the Cloncurry district, Queensland , 1998 .
[16] Geordie Mark. Petrogenesis of Mesoproterozoic K‐rich granitoids, southern Mt Angelay igneous complex, Cloncurry district, northwest Queensland , 1999 .
[17] R. Page,et al. Aspects of geochronology and crustal evolution in the Eastern Fold Belt, Mt Isa Inlier∗ , 1998 .
[18] H.,et al. Overview of the Yerington Porphyry Copper District: Magmatic to Nonmagmatic Sources of Hydrothermal Fluids, Their Flow Paths, Alteration Affects on Rocks, and Cu-Mo-Fe-Au Ores , 2007 .
[19] M. J. Rubenach,et al. Metasomatic albitites and related biotite‐rich schists from a low‐pressure polymetamorphic terrane, Snake Creek Anticline, Mount Isa Inlier, north‐eastern Australia: microstructures and P–T–d paths , 2002 .
[20] Geordie Mark,et al. The protracted hydrothermal evolution of the Mount Isa Eastern Succession: A review and tectonic implications , 2008 .
[21] W. Griffin,et al. Trace‐element signatures of apatites in granitoids from the Mt Isa Inlier, northwestern Queensland , 2001 .
[22] R. J. P. Lyon,et al. Analysis of rocks and minerals by reflected infrared radiation , 1963 .
[23] Geordie Mark,et al. Insights into the genesis and diversity of epigenetic Cu – Au mineralisation in the Cloncurry district, Mt Isa Inlier, northwest Queensland , 2006 .
[24] A. Johannsen. Eruptive Rocks, Their Genesis, Composition, Classification, and Their Relation to Ore-deposits. S. J. Shand , 2022 .
[25] P. Pollard,et al. Australian Proterozoic Iron Oxide-Cu-Au Deposits: An Overview with New Metallogenic and Exploration Data from the Cloncurry District, Northwest Queensland , 2001 .
[26] Patrick J. Williams,et al. Stable isotope evidence for magmatic fluid input during large‐scale Na–Ca alteration in the Cloncurry Fe oxide Cu–Au district, NW Queensland, Australia , 2004 .
[27] R. Kretz. Symbols for rock-forming minerals , 1983 .
[28] T. Baker,et al. Granite-related overpressure and volatile release in the mid crust: fluidized breccias from the Cloncurry District, Australia , 2006 .
[29] M. Neudert. Geology of the Mount Isa Inlier and Environs, Queensland and Northern Territory , 1990 .
[30] John B. Adams,et al. Spectral reflectance 0.4 to 2.0 microns of silicate rock powders. , 1967 .
[31] Shiqi Wang,et al. Geochemistry and origin of Proterozoic skarns at the Mount Elliott Cu–Au(–Co–Ni) deposit, Cloncurry district, NW Queensland, Australia , 2001 .
[32] R. Vincent,et al. Spectral compositional imaging of silicate rocks. , 1972 .
[33] N. Oliver,et al. High-Temperature Fluid-Rock Interaction and Scapolitization in an Extension-Related Hydrothermal System, Mary Kathleen, Australia , 1994 .
[34] D. Sherman. The electronic structures of Fe3+ coordination sites in iron oxides: Applications to spectra, bonding, and magnetism , 1985 .