Prof. Schmitt reports that model calculations demonstrated that
zircon formation is only possible over such protracted durations if the inflow of magma amounted to approx.
Not exact matches
But in order for today's magnetic intensity readings of the magnetite to reveal the actual conditions of that era, the researchers needed to make sure the magnetite within the
zircon remained pristine from the time of
formation.
One line of evidence comes from hardy crystals called
zircons, found primarily in granite — the
formation of granite requires subduction, the sinking of a lithospheric slab into the mantle where it partially melts to produce so - called granitic magma.
Equally astonishing is the time of
formation of the Tava sandstone, determined from detrital
zircon analysis: the Tava proves to be from a time period ~ 750 million years ago, which was not known to be represented in the Colorado Rockies: the Cryogenian Period.
More evidence of an earlier
formation date for the Manson crater comes from the discovery in South Dakota of flawed grains of quartz, feldspar and
zircon.
To help narrow the range of possible ages for the sandstone, Siddoway and Gehrels compared the age distributions of the Tava
zircons with the age distributions of
zircons found in other sandstone
formations in Colorado, Utah, northern Arizona, and southern California.
This is a timeline of the history of our planet places the
formation of the Jack Hills
zircon and a «cool early Earth» at 4.4 billion years.
The oldest fragment of Earth's primeval crust is a
zircon dated to be 4.4 billion years old, having formed less than 160 million years after planetary
formation (more).
As the
zircons were radioactively dated to be as old as 4.25 billion years, the new findings suggest that carbon - based life may have been present on Earth within the first 300 million years after planetary
formation, possibly as a «planetary mega-organism» in Earth's oceans (Michael Marshall, New Scientist, November 25, 2011).
To do this Trail, Watson, and their colleague, postdoctoral researcher Nicholas Tailby, recreated the
formation of
zircons in the laboratory at different oxidation levels.
A timeline of the history of our planet places the
formation of the Jack Hills
zircon and a «cool early Earth» at 4.4 billion years.
SHRIMP U — Pb
zircon geochronology of the Liaoji granitoids: Constraints on the evolution of the Paleoproterozoic Jiao - Liao - Ji belt in the Eastern Block of Petrogenesis, detrital
zircon SHRIMP U-Pb geochronology, and tectonic implications of the Upper Paleoproterozoic Seosan iron
formation, western Gyeonggi
Detrital
zircon U-Pb dating of Suining Formation sandstone from the Daba Mountains, northeastern Sichuan and its stratigraphic implications Zircon (/ ˈ z ɜːr k ɒ n / or / ˈ z ɜːr k ən /) is a mineral belonging to the group of nesosili
zircon U-Pb dating of Suining
Formation sandstone from the Daba Mountains, northeastern Sichuan and its stratigraphic implications
Zircon (/ ˈ z ɜːr k ɒ n / or / ˈ z ɜːr k ən /) is a mineral belonging to the group of nesosili
Zircon (/ ˈ z ɜːr k ɒ n / or / ˈ z ɜːr k ən /) is a mineral belonging to the group of nesosilicates.