More Evidence That the Moon Contributes to Earthquakes
http://www.theatlantic.com/science/archi...es/499637/
EXCERPT: [...] The deep tremors that can lead to major earthquakes can be very sensitive to tidal stress changes. [...] In other words, during a new moon or full moon, a small increase in tidal stress might be enough to encourage a very small fracture into a major earthquake. [...] But that’s only if the research holds up, as seismologists continue to pore over larger data sets. Not all large earthquakes are caused by the moon’s movements. But some of them might be, and so we’d do well to pay closer attention to the subtle yet powerful ways in which the moon exerts its influence on our planet, especially in regions prone to earthquakes. Scientists may have use for ancient omens yet....
New discovery shatters previous beliefs about Earth’s origin
https://www.sciencedaily.com/releases/20...134917.htm
RELEASE: A new study led by Western University's all-star cosmochemist Audrey Bouvier proves that the Earth and other planetary objects formed in the early years of the Solar System share similar chemical origins -- a finding at odds with accepted wisdom held by scientists for decades. The findings were published today by the journal Nature.
Bouvier, the Canada Research Chair (CRC) in Planetary Materials and an Isotope Cosmochemistry professor in Western's Department of Earth Sciences, made the game-changing discovery in collaboration with Maud Boyet from the Magmas and Volcanoes Laboratory at Blaise Pascal University in Clermont-Ferrand, France.
With data uncovered through thermal ionization mass spectrometry, Bouvier and Boyet demonstrated that the Earth and other extraterrestrial objects share the same initial levels of Neodymium-142 (142Nd) -- one of seven isotopes found in the chemical element neodymium -- which is widely distributed in the Earth's crust and most commonly used for magnets in commercial products like microphones and in-ear headphones.
In 2005, a small variation in 142Nd was detected between chondrites, which are stony meteorites considered essential building blocks of the Earth, and terrestrial rocks. These results were widely interpreted as an early differentiation of the interior of the Earth (including the crust and mantle) and these chondrites within the first 30 million years of its history.
These new results from Bouvier and Boyet show that these differences in 142Nd were in fact already present during the growth of Earth and not introduced later, as was previously believed.
"How the Earth was formed and what type of planetary materials were part of that formation are issues that have puzzled generations of scientists," says Bouvier, Curator of the Western Meteorite Collection and also a principal investigator at Western's Centre for Planetary Science and Exploration (CPSX). "And these new isotopic measurements of meteorites provide exciting answers to these questions about our origins and what made the Earth so special."
By using vastly improved measurement techniques, Bouvier and Boyet deduced that different meteoritical objects found in the Solar System incorporated the elements neodymium (Nd) and samarium (Sm) but with slightly different isotopic compositions. These variations in stable isotopes also show that the Solar System was not uniform during its earliest times and that materials formed from previous generations of stars were incorporated in various proportions into the building blocks of planets.
http://www.theatlantic.com/science/archi...es/499637/
EXCERPT: [...] The deep tremors that can lead to major earthquakes can be very sensitive to tidal stress changes. [...] In other words, during a new moon or full moon, a small increase in tidal stress might be enough to encourage a very small fracture into a major earthquake. [...] But that’s only if the research holds up, as seismologists continue to pore over larger data sets. Not all large earthquakes are caused by the moon’s movements. But some of them might be, and so we’d do well to pay closer attention to the subtle yet powerful ways in which the moon exerts its influence on our planet, especially in regions prone to earthquakes. Scientists may have use for ancient omens yet....
New discovery shatters previous beliefs about Earth’s origin
https://www.sciencedaily.com/releases/20...134917.htm
RELEASE: A new study led by Western University's all-star cosmochemist Audrey Bouvier proves that the Earth and other planetary objects formed in the early years of the Solar System share similar chemical origins -- a finding at odds with accepted wisdom held by scientists for decades. The findings were published today by the journal Nature.
Bouvier, the Canada Research Chair (CRC) in Planetary Materials and an Isotope Cosmochemistry professor in Western's Department of Earth Sciences, made the game-changing discovery in collaboration with Maud Boyet from the Magmas and Volcanoes Laboratory at Blaise Pascal University in Clermont-Ferrand, France.
With data uncovered through thermal ionization mass spectrometry, Bouvier and Boyet demonstrated that the Earth and other extraterrestrial objects share the same initial levels of Neodymium-142 (142Nd) -- one of seven isotopes found in the chemical element neodymium -- which is widely distributed in the Earth's crust and most commonly used for magnets in commercial products like microphones and in-ear headphones.
In 2005, a small variation in 142Nd was detected between chondrites, which are stony meteorites considered essential building blocks of the Earth, and terrestrial rocks. These results were widely interpreted as an early differentiation of the interior of the Earth (including the crust and mantle) and these chondrites within the first 30 million years of its history.
These new results from Bouvier and Boyet show that these differences in 142Nd were in fact already present during the growth of Earth and not introduced later, as was previously believed.
"How the Earth was formed and what type of planetary materials were part of that formation are issues that have puzzled generations of scientists," says Bouvier, Curator of the Western Meteorite Collection and also a principal investigator at Western's Centre for Planetary Science and Exploration (CPSX). "And these new isotopic measurements of meteorites provide exciting answers to these questions about our origins and what made the Earth so special."
By using vastly improved measurement techniques, Bouvier and Boyet deduced that different meteoritical objects found in the Solar System incorporated the elements neodymium (Nd) and samarium (Sm) but with slightly different isotopic compositions. These variations in stable isotopes also show that the Solar System was not uniform during its earliest times and that materials formed from previous generations of stars were incorporated in various proportions into the building blocks of planets.