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NARROW
GeoRef Subject
-
all geography including DSDP/ODP Sites and Legs
-
Africa
-
Madagascar (1)
-
North Africa
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Atlas Mountains
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Moroccan Atlas Mountains
-
Anti-Atlas (1)
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High Atlas (1)
-
-
-
Morocco
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Moroccan Atlas Mountains
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Anti-Atlas (1)
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High Atlas (1)
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Southern Africa
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Kaapvaal Craton (1)
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Karoo Basin (1)
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South Africa
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Merensky Reef (1)
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Asia
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Far East
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China
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North China Platform (1)
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Gangdese Belt (1)
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Lhasa Block (2)
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Japan
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Honshu
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Indus-Yarlung Zangbo suture zone (1)
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Middle East
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Zagros (1)
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Atlantic Ocean
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Australasia
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nitrogen
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noble gases
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oxygen
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Invertebrata
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framework silicates
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scapolite group
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Primary terms
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absolute age (19)
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academic institutions (2)
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Africa
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Madagascar (1)
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North Africa
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Atlas Mountains
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Moroccan Atlas Mountains
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Anti-Atlas (1)
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High Atlas (1)
-
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Morocco
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Moroccan Atlas Mountains
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Anti-Atlas (1)
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High Atlas (1)
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Southern Africa
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Kaapvaal Craton (1)
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Karoo Basin (1)
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South Africa
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Bushveld Complex (1)
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Merensky Reef (1)
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Asia
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Far East
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China
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Gangdese Belt (1)
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Lhasa Block (2)
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Japan
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Honshu
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Yamanashi Japan (1)
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India
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Dharwar Craton (1)
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Indus-Yarlung Zangbo suture zone (1)
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Middle East
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Iran
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Zagros (1)
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associations (2)
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Atlantic Ocean
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Puerto Rico Trench (1)
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Australasia
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Australia
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Queensland Australia
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Cloncurry mining district (7)
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Georgetown Inlier (1)
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Hodgkinson Province (1)
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Mount Isa Australia (6)
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Mount Isa Inlier (14)
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Mary Kathleen
The two-dimensional pattern of metamorphic fluid flow at Mary Kathleen, Australia: Fluid focusing, transverse dispersion, and implications for modeling fluid flow
Low-pressure, high-temperature metamorphism in a compressional tectonic setting; the Mary Kathleen fold belt, northeastern Australia
Sm-Nd isotope systematics in uranium rare-earth element mineralization at the Mary Kathleen uranium mine, Queensland
Chronology of magmatism, skarn formation, and uranium mineralization, Mary Kathleen, Queensland, Australia; discussion
Chronology of magmatism, skarn formation, and uranium mineralization, Mary Kathleen, Queensland, Australia; reply
Chronology of magmatism, skarn formation, and uranium mineralization, Mary Kathleen, Queensland, Australia
Mary Kathleen uranium deposit, Mount Isa-Cloncurry District, Queensland, Australia
Overview map showing the Mary Kathleen Fold Belt (grey shading) in the Moun...
Abstract Consideration of the role of rock property variations is crucial in any analysis of the effects of deformation on fluid flow and mineralization. An empirical analysis of any mineralized terrain should consider this factor, in addition to those used in any other analysis of geometry and kinematics, such as orientation, evolution of the stress and strain fields, and the known distribution of veins, shear zones, breccias, and alteration. The conceptual models that arise from such an analysis can be enhanced by computer models. The models shown here are finite difference models that simulate fluid flow in deforming rock masses, one for fluid flow along predefined rock boundaries (Universal Distinct Element Code, UDEC), and another for fluid flow through deforming porous media (Fast Lagrangian Analysis of Continua, FLAC). UDEC modeling of the perturbed stress field around stronger, lower permeability meta-intrusive rocks in the Mary Kathleen district and the Hilton mine of the Mount Isa district, northwest Queensland, reproduces the observed location of the most intense veining and alteration. FLAC modeling of the Mary Kathleen U-REE orebody reproduces the location and geometry of ore shoots and provides an explanation for focusing of regional fluid towards the ore deposition sites. FLAC models of the giant Mount Isa copper deposit reveal that the effect of the rheological heterogeneity on fluid flow and solute transport is amplified if consideration is made of whether or not the rocks are contractant or dilatant, with increasing strain. Multiple working hypotheses can be evaluated quickly by such modeling; therefore, the models can be used in exploration and orebody extension studies. Furthermore, it is suggested from our work that the size and spacing of epigenetic, structurally controlled ore deposits is related in a fairly systematic way to the scale and degree of rock property variations, at least for a given strain history. For giant ore deposits to form, it requires that the gradients in pore pressure generated at local scales by heterogeneous rock packages must be subordinate to those operating at broader scales.