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all geography including DSDP/ODP Sites and Legs
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Africa
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carbon
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GeoRef Categories
Era and Period
Epoch and Age
Date
Availability
strontium ores
GEOCHEMICAL AND MINERALOGICAL FEATURES OF GYPSUM OF THE KUNGURIAN STAGE IN THE SOUTHERN CIS-URALS ( Lower Permian ) Available to Purchase
Fluorsigaiite, Ca 2 Sr 3 (PO 4 ) 3 F, a new mineral of the apatite supergroup from the Saima alkaline complex, Liaoning Province, China Available to Purchase
ARSENIC-INDUCED DOWNSHIFT OF RAMAN BAND POSITIONS FOR PYRITE Available to Purchase
The Deccan Volcanic Province (DVP), India: A Review: Part 2: Geochemistry, petrological evolution, petrogenesis, mantle sources, age and erupted volume relations, Upper Cretaceous-Palaeogene (K-Pg) mass extinctions, economic aspects, summary and future studies in DVP Available to Purchase
Geological Introduction to Strontium-Rich Sub-soil Brine with Emphasis on the Little Rann of Kutch and Bhavnagar, Gujarat Available to Purchase
Genesis of celestite – bearing cap rock formation from the Ain Allega ore deposit (northern Tunisia): contributions from microthermometric studies Available to Purchase
Fluid inclusion microthermometry and rare earth element distribution in the celestites of the Jebel Doghra ore deposit (Dome Zone, northern Tunisia): towards a new genetic model Available to Purchase
Hydrothermal Zircon Available to Purchase
Epigenetic, low-temperature, carbonate-hosted Pb-Zn-Cu-Ba-F-Sr deposits in México: A Mississippi Valley–type classification Available to Purchase
The low-temperature epigenetic and stratabound Pb-Zn-Cu-Ba-F-Sr–bearing ore deposits enclosed within sedimentary columns historically have been major sources of metals. Exploration companies still find these deposits to be a profitable exploration target due to their simple mineralogy as well as the large tonnage that can present, always considering the mineral districts as a whole. In northeastern México, several nonmagmatic, low-temperature Pb-Zn-F-Ba deposits have been systematically considered as magmatic-related (skarns, high-temperature replacement deposits, epithermal deposits, etc.). Recently, these deposits have been restudied and placed within a scenario of deep fluid circulation of basinal brines through the Mesozoic sedimentary series, enriched in Ba, F, and metals during fluid flow and water-rock interactions. These fluids gave rise to a series of strata-bound epigenetic ore deposits scattered throughout the whole Mesozoic carbonate platform and can be shown to be unrelated to any period of magmatism. There is no intense alteration to the host rocks. Commonly there is a close association with organic matter, either liquid hydrocarbons or bitumen; they have a very simple mineralogy of barite, celestine, fluorite, sphalerite, galena, and have low formation temperatures (90–105 °C) combined with variable salinities. These characteristics make these deposits similar to the Mississippi Valley–type deposits, possibly most similar to the Alpine-Appalachian subtype.