Armstrong, R., Vishnevysky, S., Koeberl., U-Pb analyses of
zircons from the Popigai imapct structure, Russia: first results, Meteorite Imapcts in Find images, sites, tombs and tomb components through the various searches below.
The new, younger age obtained for the oldest lunar crust is similar to ages obtained for the oldest terrestrial minerals —
zircons from western Australia — suggesting that the oldest crusts on both Earth and Moon formed at approximately the same time, and that this time dates from shortly after the giant impact.
With the support of the Irish Reseach Council (IRC) and Science Foundation Ireland (SFI), the team collected thousands of
zircons from the Sudbury impact crater in Ontario, Canada.
They were understandably very happy to see that the chemistry of
the zircons from the Canadian impact crater matched the oldest crystals known to man.»
In the summer of 2014, with the support of the Irish Reseach Council (IRC) and Science Foundation Ireland (SFI), the team collected thousands of
zircons from the Sudbury impact crater, Ontario, Canada - the best preserved large impact crater on Earth and the planet's second oldest confirmed crater at almost two billion years old.
The zircons from Mauritius, it turned out, were hundreds or even thousands of millions of years old, although the island's oceanic crust was less than 10 million years old.
Professor Luca Caricchi adds: «When we determine the age of a family of
zircons from a small sample of solidified magmatic rock, using results from the mathematical model we have developed, we can tell what the size of the entire magma chamber was, as well as how fast the magma reservoir grew.»
She then searched the literature for all comparable analyses of Hadean zircon and for representative analyses of
zircon from other modern environments.
Measurements on some 50 grains of
zircon from the gneiss rocks found in Canada showed them to be 3.962 billion years old, with a margin of error of only three million years.
Not exact matches
Perth - based explorer Image Resources has entered into an agreement for the purchase of a wet concentration plant, and an offtake deal for product
from its Boonanarring mineral sands project near Gingin, with a Chinese
zircon company to emerge as a major shareholder.
Called TiZir, the joint venture was formed in 2011 with Limb's business contributing the mineral sands mine and initial processing infrastructure that separates the heavy metals extracted
from the sand into materials such as
zircon, rutile and ilmenite.
«If the earth formed over four billion years ago, all helium should have escaped
from zircons, yet the crystals are loaded with this element» «The atmosphere should be full of helium atoms, the byproducts of millions of years of radioisotope decay, but it isn't.»
«The astonishing result was that the ages of the
zircons measured
from all five of the smaller volcanoes extended continuously
from the time of the eruption 75,000 years ago back to the last supervolcanic eruption.»
The paper, Use and abuse of
zircon - based thermometers: A critical review and a recommended approach to identify antecrystic
zircons, also proposes an efficient and integrated approach to assist in identifying
zircons and evaluating
zircon components sourced
from older rocks.
Tarduno's new results are based on the record of magnetic field strength fixed within magnetite found within
zircon crystals collected
from the Jack Hills of Western Australia.
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.
Sarah Crespi talks to Allison Rubin about what we can learn
from zircon crystals outside of a volcano about how long hot magma hangs out under a volcano.
Another group, led by MIT's Benjamin Weiss, collected rocks
from the same area of the Jack Hills but says the
zircon, although old, may not have been magnetized billions of years ago.
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.
The team were also able to determine where the original material in the river came
from by dating mineral grains such as
zircon and mica, revealing the previous course of the river.
Wayne Premo and Glenn Izett of the US Geological Survey in Denver estimated that
zircon crystals
from an impact layer in North America were 33 to 55 million years old.
To better understand the cycle of magma production, the researchers analyzed oxygen isotope ratios in quartz and
zircon, water - and heat - resistant minerals,
from volcanic rocks in the Yellowstone caldera.
«
Zircons crystallize out of molten rocks with special compositions, and their appearance signifies a profound change
from silica - poor to silica - rich volcanism.
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.
The researchers, led by Elizabeth Bell — a postdoctoral scholar in Harrison's laboratory — studied more than 10,000
zircons originally formed
from molten rocks, or magmas,
from Western Australia.
«We discovered that Icelandic
zircons are quite distinctive
from crystals formed in other locations on modern Earth.
The chemical make - up of the
zircon crystals suggests that the magma they cooled
from was generated by the melting of a mud - rich sediment, which is the sort of environment in which organic remains might accumulate.
We also found that they formed in magmas that are remarkably different
from those in which the Hadean
zircons grew,» said Carley.
This alternate view of Earth's first geologic eon, called the Hadean, has gained substantial new support
from the first detailed comparison of
zircon crystals that formed more than 4 billion years ago with those formed contemporaneously in Iceland, which has been proposed as a possible geological analog for early Earth.
Working with Miller and doctoral student Abraham Padilla at Vanderbilt, Joe Wooden at Stanford University, Axel Schmitt and Rita Economos
from UCLA, Ilya Bindeman at the University of Oregon and Brennan Jordan at the University of South Dakota, Carley analyzed about 1,000
zircon crystals for their age and elemental and isotopic compositions.
Professor of Earth and Environmental Sciences at Vanderbilt University, and published online this weekend by the journal Earth and Planetary Science Letters in a paper titled, «Iceland is not a magmatic analog for the Hadean: Evidence
from the
zircon record.»
Tiny minerals called
zircons have also survived
from the early Earth.
Portrait of a young planet The Jack Hills
zircons show that a magnetic field existed as early as 4 billion years ago, fluctuating in strength
from a value similar to today's — around 25 microteslas — to about 12 % of that.
The new study confirms that
zircon crystals
from Western Australia's Jack Hills region crystallized 4.4 billion years ago, building on earlier studies that used lead isotopes to date the Australian
zircons and identify them as the oldest bits of the Earth's crust.
4 The oldest known pieces of our planet's surface are 4.4 - billion - year - old
zircon crystals
from the Jack Hills of western Australia.
The
zircons analyzed by Humayun's team were
from Black Beauty samples kept in Paris.
McKenzie assembled
zircon counts
from rocks laid down in the last 3 billion years,
from all around the world.
McKenzie's new evidence comes
from tiny
zircon crystals.
However, we can only go back in time so far, as the only material we have
from the very early Earth comes in the form of tiny, naturally occurring
zircon crystals.
Eventually, a stable rocky crust may have developed between Years 0.2 and 0.4 billion (see J. Bret Bennington's discussion of recycled
zircons (crystals of zirconium silicate)
from the rocks of western Australia in the Hadean Eon and the January 11, 2001 announcement of
zircons found north of Perth that appear to be 4.4 billion years old), covered and surrounded by soupy water that was already rich with organic compounds
from interstellar space.
To test this idea, researchers
from Trinity College Dublin decided to study a much younger impact crater to see if
zircon crystals similar to the very old ones could possibly have formed in these violent settings.
Zircon contains lead, and this element can be removed
from the mineral as it is melted and re-shaped by impacts.
Shellnutt (2017), in a succinct review of the Panjal Traps (c. 290 Ma), an important component of the Himalayan magmatic province, discusses the synchronous nature of basalts, that chemically range
from continental tholeiite to ocean - floor basalt, and crustally derived silicic volcanic rocks (rhyolites and trachytes: 206Pb / 238U
zircon in situ age of 289 ± 3 Ma), that developed in a shallow lithospheric rift with significant mingling between crustal melts and mafic magmas.
For the study, they looked at data for roughly 120,000
zircon grains
from thousands of samples across the globe.
To Mojzsis, the message
from the most ancient
zircons is this: just 50 million years after a mammoth impact formed the moon, Earth had conditions we might recognize today, not the hellish conditions long favored by the conventional viewpoint.
«
From the Hadean
zircons we can understand further what the thermal consequences for the crust were, and test our models for habitability during the late heavy bombardment.
With support
from a NASA Exobiology grant, Mojzsis has begun examining the effect of impacts on a new batch of
zircons found in areas that have been hit by more recent impacts.
In addition to rocky asteroids and icier bodies further out
from the Sun, many agglomerated into larger planetesimals that eventually collided to form planets like the Earth, and more than 250 minerals, including olivine and
zircon, developed within the planetesimals with the help of melting, collisional shocks, and reactions with water.
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From opening to subduction of an oceanic domain constrained by LA - ICP - MS U-Pb
zircon dating (Variscan belt, Southern Armorican Massif, France)