The main result of this research, is that the variations of the flux, as predicted from the galactic model and as observed
from the Iron meteorites is in sync with the occurrence of ice - age epochs on Earth.
It showed that the concentrations of metals, including iron, nickel, cobalt and chromium, matched the values known
from iron meteorites.
Geologist Matthew Pasek of the University of Arizona in Tucson, who previously studied the possibility that early life used phosphorus
from iron meteorites, knew that cloud - to - ground lightning was one of the few natural phenomena that could produce enough energy to create phosphite.
Not exact matches
The amount of nickel - 60 found in
meteorite samples — particularly in comparison to the amount of stable, «ordinary»
iron - 56 — can indicate how much
iron - 60 was present when the larger parent body
from which the
meteorite broke off was formed.
Known as the «
iron man,» a 24 - centimeter - high sculpture was likely created
from a piece of the Chinga
meteorite that was strewn across the border region between Russia and Mongolia between 10,000 and 20,000 years ago
Iron meteorites, derived
from the shattered cores of larger asteroids, reach Earth only rarely.
«Having looked at some of the published trace element data for this artefact, it looks pretty convincing to me that this is very likely originated
from Chinga
iron meteorite,» says Meenakshi Wadhwa, director of the Center for Meteorite Studies at Arizona State University
meteorite,» says Meenakshi Wadhwa, director of the Center for
Meteorite Studies at Arizona State University
Meteorite Studies at Arizona State University in Tempe.
An
iron and silicate
meteorite is thought to resemble the raw material
from which the core formed.
By looking at tungsten and molybdenum isotopes on
iron meteorites, the team, made up of scientists
from Lawrence Livermore National Laboratory and Institut für Planetologie at the University of Münsterin Germany, found that
meteorites are made up
from two genetically distinct nebular reservoirs that coexisted but remained separated between 1 million and 3 - 4 million years after the solar system formed.
If the Martian core is dense (composed of
iron) similar to Earth's or SNC
meteorites thought to originate
from Mars, then the minimum core radius would be about 1300 kilometers.
Laser - zapping of a globular, golf - ball - size object on Mars by NASA's Curiosity rover confirms that it is an
iron - nickel
meteorite fallen
from the Red Planet's sky.
This finding was expected because
meteorites from Vesta have less
iron than the solar nebula
from which planetary building blocks formed.
A weapon as legendary as the dagger of King Tutankhamun needs an epic backstory, and last year X-ray analysis showed that the
iron in the blade came
from meteorites.
Bronze Age artifacts revealed nickel levels and ratio of
iron to cobalt that suggest these were made using metals
from meteorites.
``... we lack compelling scenarios leading to the origin of
iron meteorites... Early solar system collisions have been called upon to excavate this
iron [
from the cores of the largest asteroids], although numerical impact models have found this task difficult to achieve, particularly when it is required to occur many dozens of times, yet not a single time for asteroid Vesta.»
The exhibition also includes important pieces
from across Parker's career, such as Cold Dark Matter; An Exploded View (1991), and opens with a breathtaking firework display that will send fragments of
iron meteorite up into the skies above Manchester.
Shaviv, N., Cosmic ray diffusion
from the galactic spiral arms,
iron meteorites, and a possible climate connection?
N. Shaviv, «Cosmic Ray Diffusion
from the Galactic Spiral Arms,
Iron Meteorites, and a Possible Climatic Connection», Physical Review Letters 89, 051102, (2002).
The so - called «Galactic Cosmic Rays» probably come directly
from the Sun's pulsar core, and were recorded as a gradient in cosmic ray exposures of
meteorites at the birth of the solar system:
iron meteorites > stone
meteorites > carbonaceous chondrites
Researchers have found that an
iron - containing mineral called dusty olivine, present in
meteorites, retains a record of the magnetic field
from the early solar system around 4.6 billion years ago.