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{"type":"standard","title":"Narryer Gneiss terrane","displaytitle":"Narryer Gneiss terrane","namespace":{"id":0,"text":""},"wikibase_item":"Q6966352","titles":{"canonical":"Narryer_Gneiss_terrane","normalized":"Narryer Gneiss terrane","display":"Narryer Gneiss terrane"},"pageid":3439693,"thumbnail":{"source":"https://upload.wikimedia.org/wikipedia/commons/thumb/d/d7/Jack_Hills%2C_Western_Australia_%28Landsat_5_TM%2C_2009-07-14%2C_detail%29.jpg/330px-Jack_Hills%2C_Western_Australia_%28Landsat_5_TM%2C_2009-07-14%2C_detail%29.jpg","width":320,"height":226},"originalimage":{"source":"https://upload.wikimedia.org/wikipedia/commons/d/d7/Jack_Hills%2C_Western_Australia_%28Landsat_5_TM%2C_2009-07-14%2C_detail%29.jpg","width":1772,"height":1253},"lang":"en","dir":"ltr","revision":"1284064742","tid":"cbb12a1b-1205-11f0-9112-1927ceb3a3a7","timestamp":"2025-04-05T10:07:35Z","description":"Geological complex of ancient rocks in Western Australia","description_source":"local","content_urls":{"desktop":{"page":"https://en.wikipedia.org/wiki/Narryer_Gneiss_terrane","revisions":"https://en.wikipedia.org/wiki/Narryer_Gneiss_terrane?action=history","edit":"https://en.wikipedia.org/wiki/Narryer_Gneiss_terrane?action=edit","talk":"https://en.wikipedia.org/wiki/Talk:Narryer_Gneiss_terrane"},"mobile":{"page":"https://en.m.wikipedia.org/wiki/Narryer_Gneiss_terrane","revisions":"https://en.m.wikipedia.org/wiki/Special:History/Narryer_Gneiss_terrane","edit":"https://en.m.wikipedia.org/wiki/Narryer_Gneiss_terrane?action=edit","talk":"https://en.m.wikipedia.org/wiki/Talk:Narryer_Gneiss_terrane"}},"extract":"The Narryer Gneiss terrane is a geological complex in Western Australia that is composed of a tectonically interleaved and polydeformed mixture of granite, mafic intrusions and metasedimentary rocks in excess of 3.3 billion years old, with the majority of the Narryer Gneiss terrane in excess of 3.6 billion years old. The rocks have experienced multiple metamorphic events at amphibolite or granulite conditions, resulting in often complete destruction of original igneous or sedimentary (protolith) textures. Importantly, it contains the oldest known samples of the Earth's crust: samples of zircon from the Jack Hills portion of the Narryer Gneiss have been radiometrically dated at 4.4 billion years old, although the majority of zircon crystals are about 3.6-3.8 billion years old.","extract_html":"
The Narryer Gneiss terrane is a geological complex in Western Australia that is composed of a tectonically interleaved and polydeformed mixture of granite, mafic intrusions and metasedimentary rocks in excess of 3.3 billion years old, with the majority of the Narryer Gneiss terrane in excess of 3.6 billion years old. The rocks have experienced multiple metamorphic events at amphibolite or granulite conditions, resulting in often complete destruction of original igneous or sedimentary (protolith) textures. Importantly, it contains the oldest known samples of the Earth's crust: samples of zircon from the Jack Hills portion of the Narryer Gneiss have been radiometrically dated at 4.4 billion years old, although the majority of zircon crystals are about 3.6-3.8 billion years old.
"}