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Crystals On Meteorite Reveal Clues To Early Solar System Evolution

Date:
August 4, 2007
Source:
University Of Toronto
Summary:
A new study has uncovered tiny zircon crystals in a meteorite originating from Vesta (a large asteroid between Mars and Jupiter) shedding light on the formation of planetesimals, small astronomical objects that form the basis of planets. To date, studying zircons in eucrites -- meteorites formed by volcanic activity -- has been difficult due to impact- induced fracturing and their small size, typically less than five microns.
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To date, studying zircons in eucrites – meteorites formed by volcanic activity – has been difficult due to impact- induced fracturing and their small size, typically less than five microns. Most eucrites are formed within the asteroid belt that orbits Mars and Jupiter, a heap of astronomical debris from the earliest epoch of the solar system. In a study published in the recent issue of Science, researchers collected samples from eucrites found in Antarctica believed to have originated from Vesta. The researchers used new technology to reveal that asteroid’s boiling rock turned solid and crystallized within less than 10 million years of solar system formation.

samples from eucrites found in Antarctica believed to have originated from Vesta. The researchers used new technology to reveal that asteroid’s boiling rock turned solid and crystallized within less than 10 million years of solar system formation.

“Until now we have not been able to determine this time frame unambiguously,” says lead author Professor Gopalan Srinivasan of U of T’s Department of Geology. “By pinpointing the timeframe we’re able to add one more piece to the geological and historical map of our solar system.”

Scientists believe that at some point Vesta was quickly heated and then melted into a metallic and silicate core, a similar process that happened on the Earth. The energy for this process was released from the radioactive decay that was present in abundance in the early solar system. What has been unclear is when this process occurred.

Equipped with the ion microprobe at the Swedish National Museum, Srinivasan and colleagues from four institutions set to analyze the zircons in the eucrites, which formed when a radioactive element – hafnium-182 – was still alive. Radioactive hafnium-182 decays to another element – tungsten-182 – with a nearly 9 million year half-life span. By studying zircons for their 182 tungsten abundance, the researchers were able to determine the crystallization ages of eucrites occurred within that timeframe.

“Zircons on Earth and in space have basically the same characteristics,” Srinivasan says. “They occur when boiling rock crystallizes and turns into solid form primary crystallization products or they could be secondary products caused by heating from impacts. We know Vesta became inactive within first 10 million years of solar system formation which is nearly 4.5 billion years ago. This provides a snapshot of the early solar system and clues to the early evolution of Earth’s mantle and core.”


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The above post is reprinted from materials provided by University Of Toronto. Note: Materials may be edited for content and length.


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University Of Toronto. "Crystals On Meteorite Reveal Clues To Early Solar System Evolution." ScienceDaily. ScienceDaily, 4 August 2007. <www.sciencedaily.com/releases/2007/08/070803140904.htm>.
University Of Toronto. (2007, August 4). Crystals On Meteorite Reveal Clues To Early Solar System Evolution. ScienceDaily. Retrieved June 30, 2015 from www.sciencedaily.com/releases/2007/08/070803140904.htm
University Of Toronto. "Crystals On Meteorite Reveal Clues To Early Solar System Evolution." ScienceDaily. www.sciencedaily.com/releases/2007/08/070803140904.htm (accessed June 30, 2015).

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