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Filling a copper sample tube, in duplicate, that is used for noble gas analysis, helium and neon analyses, and determination of the 3He/4He.
The Paleoproterozoic Cu-Au deposits are commonly hosted within Neoarchean IOCG alteration systems and the common occurrence of potassic alteration especially biotite in both types of deposits means that special care is required in interpreting the paragenesis of alteration in both types of deposits. The Paleoproterozoic Cu-Au deposits are reduced, and sulfur- and quartz-rich deposits lacking in major amounts of iron oxides and are therefore unlike IOCG deposits.
This is a preview of subscription content, log in to check access. Rent this article via DeepDyve. Can Mineral — Lithos — Int Geology Rev — Google Scholar. Mineral Deposita — J Geophys Res 92 B9 —
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Dating with Isotopes Mark Williams, cu-boulder age-dating basics. Download 3. Despite the prevalent use of this term, isotope hydrologists understand that the water sample measured represents the integrated travel time through that aquifer or other water body “age” and “mean residence time” are used interchangeably.
The Copper Lake area of mainland Nova Scotia is one of several vein-controlled mineralized Cu-Au-Co systems associated with widespread carbonate and iron-oxide alteration proximal to the east-trending Cobequid-Chedabucto Fault System. Although this mineralization has been known for decades, its metallogenic affinity remains poorly defined, and in recent years an IOCG iron oxide-copper-gold model has been suggested.
In order to determine the age of mineralization and provide an important time constraint for developing a metallogenic model, direct dating of the mineralization and associated alteration was undertaken. At Copper Lake, mineralization occurs in a set of sulphide-carbonate fissure veins hosted by fine-grained metasedimentary rocks of the Middle Devonian Guysborough Group. Dating of the sulphide-alteration pyrite and phyllic-alteration muscovite stages of the ore system utilized the Re-Os and [sup.
The two different chronometers yield ages of about Ma and provide an absolute age for the mineralization. The Th-Pb dating ofmonazite indicates that rare-earth element mobility accompanied mineralization.
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The Bondar Hanza porphyry Cu deposit, hosted by a granitoid stock, is located km south of Kerman city in the elongated NW–SE trending.
A new high-tech analysis led by a University of Colorado Boulder researcher shows the oldest known petroglyphs in North America, which are cut into several boulders in western Nevada, date to at least 10, years ago and perhaps even as far back as 14, years ago. The petroglyphs located at the Winnemucca Lake petroglyph site 35 miles northeast of Reno consist of large, deeply carved grooves and dots forming complex designs on several large limestone boulders that have been known about for decades, said CU-Boulder researcher Larry Benson, who led the new effort.
Although there are no people, animals or handprint symbols depicted, the petroglyph designs include a series of vertical, chain-like symbols and a number of smaller pits deeply incised with a type of hard rock scraper. Benson and his colleagues used several methods to date the petroglyphs, including determining when the water level the Winnemucca Lake subbasin–which back then was a single body of water connecting the now-dry Winnemucca Lake and the existing Pyramid Lake–reached the specific elevation of 3, feet.
The elevation was key to the study because it marked the maximum height the ancient lake system could have reached before it began spilling excess water over Emerson Pass to the north. When the lake level was at this height, the petroglyph-peppered boulders were submerged and therefore not accessible for carving, said Benson, an adjunct curator of anthropology at the University of Colorado Museum of Natural History.
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The Qiushuwan Cu-Mo deposit is an important porphyry-skarn type Cu-Mo deposit in the East Qinling. Six samples of molybdenite for Re-Os isotopic dating are.
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