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The world ’s big iron ore repository organize when the ancient supercontinent Columbia broke up around 1.4 billion days ago , a new work suggests .

The deposits , located in what is now Hamersley Province in Western Australia , sit down on a chunk of Earth ’s crust known as the Pilbara Craton . The Pilbara Craton is one of only two pieces of crust known to engagement back to the Archaean Eon ( 3.8 billion to 2.5 billion class ago ) and host some of the honest-to-goodness stone on our satellite . ( The other archean incrustation is the Kaapvaal Craton in southern Africa . )

A cross section of a drilling core shows deep blue iron ore from the Hamersley Province.

A core of 1.3 billion-year-old deep blue iron ore from the Hamersley Province.

Rocks in the Pilbara Craton have witnessed thebirth and breakup of several supercontinents , meaning they harbour hint about the ancestry of the region ’s plenteous mineral deposits , researchers said in the newfangled study . In especial , the breakup of supercontinent Columbia , which existed between 1.7 billion and 1.45 billion year ago , and the subsequent amalgamation of Australia between 1.4 billion and 1.1 billion years ago , could explain how huge iron ore reserves constitute in the Hamersley Province .

The squad revealed its findings in a discipline published July 23 in the journalPNAS .

" The free energy from this epic geological activity in all probability triggered the product of billions of tons of iron - rich rock across the Pilbara , " field of study lead authorLiam Courtney - Davies , a geochronologist and postdoctoral associate at the University of Colorado , Boulder , said in astatement .

Satellite image of the Pilbara Craton in Western Australia shows a yellow and red coastline as seen from above next to a deep-blue ocean

A satellite image of the Pilbara Craton in Western Australia.

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The Hamersley Province holdsmore than 55 billion tons ( 50 metric gigatons ) of branding iron ore , which geologists antecedently remember formed around 2.2 billion years ago . But based on verbatim date technique , the new study find the deposit are actually much younger than that , forming between 1.4 billion and 1.1 billion years ago .

To nail the age of the deposits , Courtney - Davies and his colleagues dated mineral in eight banded iron formation — giant blocks of aqueous sway that feature tack layers of iron oxides , such as magnetic iron-ore and hematite , and iron - poor minerals like chert . The researcher used a young geochronology technique that regard analyzing uranium and lead isotope within iron oxide in the rock ‘n’ roll , which give investigator the first ever unmediated old age measure for the Hamersley Province deposits .

An animation of Pangaea breaking apart

The measurements revealed the smoothing iron ore formed around the same sentence that supercontinent Columbia , also know as Nuna , was breaking up to give hike to aprimitive Australian continent .

" Our inquiry indicates these alluviation formed in conjunction with major tectonic events , " study co - authorMartin Danisik , an associate professor of geology at Curtin University in Australia , said in the statement .

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These tectonic case would have take position across the total Pilbara Craton , providing the huge sum of money of energy required and forcing enough mineral - rich fluid from deep underground to make the monolithic deposits , harmonise to the field of study .

Cross section of the varying layers of the earth.

The finding could help geologists locate other iron deposit in the future . smoothing iron ore is an crucial factor in theproduction of iron and steel . As such , resource geographic expedition companies are always searching for unexampled iron ore deposits that they can mine .

" The uncovering of a link between these gargantuan iron ore deposit and changes in supercontinent oscillation heighten our apprehension of ancient geologic processes and improves our power to forecast where we should search in the future , " Courtney - Davies said .

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