Schechtman's work on quasicrystals in the 1980s was initially treated with skepticism and derision by colleagues, who argued quasicrystals were not possible, but since then a variety of them have been made under controlled conditions in the lab.
The new samples were found in an area that does not have the extreme pressure needed to produce them, strengthening the case that they were brought to earth about 15,000 years ago by a meteorite that was formed 4.5 billion years ago at the beginning of the solar system, the researchers said.
Steinhardt says the discovery of natural quasicrystals will raise many questions for geologists.
"How did the quasicrystal form so perfectly inside a complex meteorite when we normally have to work hard in the laboratory to get anything as perfect?" said Steinhardt.
"At the moment, we are at the tip of the iceberg," he said.
The paper based on the expedition is published this week in the UK scientific journal Reports on Progress in Physics.
(Editing by Susan Fenton)
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