Please use this identifier to cite or link to this item: http://cmuir.cmu.ac.th/jspui/handle/6653943832/57886
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dc.contributor.authorT. Loylipen_US
dc.contributor.authorS. Wannawichianen_US
dc.date.accessioned2018-09-05T03:52:35Z-
dc.date.available2018-09-05T03:52:35Z-
dc.date.issued2017-10-20en_US
dc.identifier.issn17426596en_US
dc.identifier.issn17426588en_US
dc.identifier.other2-s2.0-85034091663en_US
dc.identifier.other10.1088/1742-6596/901/1/012005en_US
dc.identifier.urihttps://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=85034091663&origin=inwarden_US
dc.identifier.urihttp://cmuir.cmu.ac.th/jspui/handle/6653943832/57886-
dc.description.abstract© Published under licence by IOP Publishing Ltd. A meteorite is a fragment of pure stone, iron or the mixture of stony-iron. The falling of meteorites into Earth's surface is part of Earth's accretion process from dust and rocks in our solar system. When these fragments come close enough to the Earth to be attracted by its gravity, they may fall into the Earth. Following the detection of objects that fall from the sky onto a home in Phitsanulok in June 27, the meteorites were analyzed by scanning electron microscopy coupled with energy dispersive X-ray spectroscopy (SEM/EDS) instruments. The results from SEM/EDS analysis show that the meteorites are mainly composed of Fe-Ni and Fe-s. The meteorite is Achondrite, a class of meteorite which does not contain Chondrule. The meteorites in this work are thought to be part of a large asteroid.en_US
dc.subjectPhysics and Astronomyen_US
dc.titleElemental composition analysis of stony meteorites discovered in Phitsanulok, Thailanden_US
dc.typeConference Proceedingen_US
article.title.sourcetitleJournal of Physics: Conference Seriesen_US
article.volume901en_US
article.stream.affiliationsChiang Mai Universityen_US
article.stream.affiliationsNational Astronomical Research Institute of Thailanden_US
Appears in Collections:CMUL: Journal Articles

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