the federal govt of nigeria has made a budget of oil exploration in some part of nigeria state which are lake chad, yola, anambra, bauchi and benue. the project is to commence in 2013 and the budget worth #49bn for research and exploiration
Friday, 12 October 2012
Super-Earth Planet Likely Made of Diamond
Move over, Hope Diamond. The most famous gems on Earth have new competition in the form of a planet made largely of diamond, astronomers say.
The alien planet, a so-called "super-Earth," is called 55 Cancri e and was
discovered in 2004 around a nearby star in our Milky Way galaxy. After
estimating the planet's mass and radius, and studying its host star's
composition, scientists now say the rocky world is composed mainly of
carbon (in the form of diamond and graphite), as well as iron, silicon
carbide, and potentially silicates. At least a third of the planet's mass is likely pure diamond.
"This is our first glimpse of a rocky world with a fundamentally different chemistry from Earth,"
lead researcher Nikku Madhusudhan of Yale University said in a
statement. "The surface of this planet is likely covered in graphite and
diamond rather than water and granite."55 Cancri e is the first likely "diamond planet" to be identified around a sun-like star, though such worlds have been theorized before. Planets like this are vastly different from our Earth, which has relatively little carbon.
"By contrast, Earth’s interior is rich in oxygen, but extremely poor in carbon — less than a part in thousand by mass," said study co-author and Yale geophysicist Kanani Lee.
55 Cancri e is what's known as a super-Earth, with a radius twice as wide as that of our own planet, and a mass eight times greater. It speeds around its host star, making a full orbit in just 18 hours (Earth takes 365 days). It is so close in to the star that its surface temperature reaches a scorching 3,900 degrees Fahrenheit (2,100 degrees Celsius), making it probably way too hot for life. [Oozing Super-Earth: Images of Alien Planet 55 Cancri e]
Previous studies of this planet suggested it might actually be covered with oozing "supercritical fluids" — high-pressure liquid-like gases — seeping out from its rocks. But this idea was based on the assumption that 55 Cancri e had a similar chemical makeup as Earth, Madhusudhan said. The new findings suggest the planet has no water at all.
The revelation of the planet's diamond nature means that it could have very different thermal evolution and plate tectonics processes than Earth, which could create bizarre types of volcanism, seismic activity, and mountain formation.
55 Cancri e is one of five planets encircling a sun-like star called 55 Cancri, which lies about 40 light-years from Earth in the constellation of Cancer. This star is so close it is visible to the naked eye in the night sky.
The researchers hope to make follow-up observations of this star system to better determine the star's composition and to analyze 55 Cancri e's atmosphere. This information could bolster the idea that the planet is a diamond world.
Wednesday, 3 October 2012
Friday, 28 September 2012
marement: More Articles Monitoring brain activity during s...
marement: More Articles Monitoring brain activity during s...: Large earthquakes can alter seismicity patterns across the globe in very different ways, according to two new studies by U.S. Geological ...
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Large earthquakes can alter seismicity patterns across the globe
in very different ways, according to two new studies by U.S. Geological
Survey seismologists. Both studies shed light on more than a decade of
debate on the origin and prevalence of remotely triggered earthquakes.
Until now, distant but damaging "aftershocks" have not been included in
hazard assessments, yet in each study, changes in seismicity were
predictable enough to be included in future evaluations of earthquake
hazards.
In a study published in this week's issue of "Nature," USGS seismologist Fred Pollitz and colleagues analyzed the unprecedented increase in global seismic activity triggered by the Magnitude-8.6 East Indian Ocean quake of April 11, 2012, and in a recently published study in the "Proceedings of the National Academy of Sciences," seismologist Volkan Sevilgen and his USGS colleagues investigated the near-cessation of seismic activity up to 250 miles away caused by the 2004 M9.2 Sumatra earthquake.
While aftershocks have traditionally been defined as those smaller earthquakes that happen after and nearby the main fault rupture, scientists now recognize that this definition is wrong. Instead, aftershocks are simply earthquakes of any size and location that would not have taken place had the main shock not struck.
"Earthquakes are immense forces of nature, involving complex rock physics and failure mechanisms occurring over time and space scales that cannot be recreated in a laboratory environment," said USGS Director Marcia McNutt. "A large, unusual event such as the East Indian earthquake last April is a once-in-a-century opportunity to uncover first order responses of the planet to sudden changes in state of stress that bring us a little closer to understanding the mystery of earthquake generation."
The East Indian Ocean event was the largest - by a factor of 10 - strike-slip earthquake ever recorded (the San Andreas is perhaps the most famous strike-slip fault). "Most great earthquakes occur along subduction zones and involve large vertical motions. No other recorded earthquake triggered as many large earthquakes elsewhere around the world as this one," said Pollitz, "probably because strike-slip faults around the globe were more responsive to the seismic waves produced by a giant strike-slip temblor."
Another clue in the six days of global aftershocks following the M8.6 quake is that the rate of global quakes during the preceding 6-12 days was extremely low. "Imagine an apple tree, with apples typically ripening and then falling at some steady rate," Stein said. "If a week goes by without any falling, there will be more very ripe apples on the tree. Now shake the trunk, and many more than normal might drop."
The authors emphasize that the week of global triggering seen after the East Indian Ocean quake has no bearing on the hypothesis advanced by others that the 2004 M9.2 Sumatra, 2010 M8.8 Maule, Chile, and 2011 M9.0 Tohoku, Japan, are related to each other. Instead, the effect of increased earthquakes lasted a week-not a decade.
The authors investigated two possible causes for the changes in remote seismicity rates: the dynamic stresses imparted by the main shock rupture, which best explain the global triggering in the April 2012 quake case; and the small but permanent stress changes, which best explain this one. The authors found that the main shock brought the transform fault segments about ¼ bar of pressure farther from static failure, and the rift segments about ¼ bar closer to static failure (for comparison, car tires are inflated with about 3 bars of pressure), which matches the seismic observations.
Incorporating the probability of aftershocks into the hazard
assessment of an area is important because the damage of even a moderate
aftershock sometimes exceeds that wrought by the main event. For
example, a M6.3 aftershock five months after the M7.1 New Zealand
earthquake in 2010 hit a more populated area, causing 181 deaths and
tripling the insured property damage of the main event.
In a study published in this week's issue of "Nature," USGS seismologist Fred Pollitz and colleagues analyzed the unprecedented increase in global seismic activity triggered by the Magnitude-8.6 East Indian Ocean quake of April 11, 2012, and in a recently published study in the "Proceedings of the National Academy of Sciences," seismologist Volkan Sevilgen and his USGS colleagues investigated the near-cessation of seismic activity up to 250 miles away caused by the 2004 M9.2 Sumatra earthquake.
While aftershocks have traditionally been defined as those smaller earthquakes that happen after and nearby the main fault rupture, scientists now recognize that this definition is wrong. Instead, aftershocks are simply earthquakes of any size and location that would not have taken place had the main shock not struck.
"Earthquakes are immense forces of nature, involving complex rock physics and failure mechanisms occurring over time and space scales that cannot be recreated in a laboratory environment," said USGS Director Marcia McNutt. "A large, unusual event such as the East Indian earthquake last April is a once-in-a-century opportunity to uncover first order responses of the planet to sudden changes in state of stress that bring us a little closer to understanding the mystery of earthquake generation."
Global aftershock study: April 2012: East Indian Ocean quake triggers many distant quakes
An extraordinary number of earthquakes of M4.5 and greater were triggered worldwide in the six days after the M8.6 East Indian Ocean earthquake in April 2012. These large and potentially damaging quakes, occurring as far away as Mexico and Japan, were triggered within days of the passage of seismic waves from the main shock that generated stresses in Earth's crust.The East Indian Ocean event was the largest - by a factor of 10 - strike-slip earthquake ever recorded (the San Andreas is perhaps the most famous strike-slip fault). "Most great earthquakes occur along subduction zones and involve large vertical motions. No other recorded earthquake triggered as many large earthquakes elsewhere around the world as this one," said Pollitz, "probably because strike-slip faults around the globe were more responsive to the seismic waves produced by a giant strike-slip temblor."
Another clue in the six days of global aftershocks following the M8.6 quake is that the rate of global quakes during the preceding 6-12 days was extremely low. "Imagine an apple tree, with apples typically ripening and then falling at some steady rate," Stein said. "If a week goes by without any falling, there will be more very ripe apples on the tree. Now shake the trunk, and many more than normal might drop."
The authors emphasize that the week of global triggering seen after the East Indian Ocean quake has no bearing on the hypothesis advanced by others that the 2004 M9.2 Sumatra, 2010 M8.8 Maule, Chile, and 2011 M9.0 Tohoku, Japan, are related to each other. Instead, the effect of increased earthquakes lasted a week-not a decade.
Sumatra quake affects faults up to 250 miles away
While global triggering of large aftershocks appears very rare, regional triggering is common and important to understand for post-main shock emergency response and recovery. Sevilgen and his USGS colleagues studied the largest quake to strike in 40 years to understand just how great the reach is on aftershock occurrence. After the M9.2 earthquake in Sumatra in 2004, aftershocks larger than M4.5 ceased for five years along part of a distant series of linked faults known as the Andaman back arc fault system. Along a larger segment of the same system, the sideways-slipping transform earthquakes decreased by two-thirds, while the rate of rift events - earthquakes that happen on a spreading center - increased by 800 percent, according to Sevilgen and his colleagues at the USGS. These very large, but distant seismicity rate changes are unprecedented.The authors investigated two possible causes for the changes in remote seismicity rates: the dynamic stresses imparted by the main shock rupture, which best explain the global triggering in the April 2012 quake case; and the small but permanent stress changes, which best explain this one. The authors found that the main shock brought the transform fault segments about ¼ bar of pressure farther from static failure, and the rift segments about ¼ bar closer to static failure (for comparison, car tires are inflated with about 3 bars of pressure), which matches the seismic observations.
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