The"Boring Billion"refers the era between c.1.8 and 0.8 billion years ago(Ga)(Holland,2006;Young,2013).Especially,the period from 1.6 to 1.0 Ga is known as"the dullest time in Earth’s deep-time history...The"Boring Billion"refers the era between c.1.8 and 0.8 billion years ago(Ga)(Holland,2006;Young,2013).Especially,the period from 1.6 to 1.0 Ga is known as"the dullest time in Earth’s deep-time history"(Buick et al.,1995).The reason why this period is referred to as the"Boring Billion"is because there were very few’special’or’interesting’events discovered in the geological or geochemical records over nearly one-fourth of Earth's deep-time history.展开更多
Tectonic evolution and paleogeography of the two major continental blocks Fennoscandia and VolgoSarmatia during their docking to form the East European Craton(Baltica)at 1.8–1.7 Ga represent important‘puzzle
There are only two quantitative tools for Precambrian paleogeographic reconstructions–paleomagnetic data and dyke swarms geometries.Paleomagnetic data provide information about paleolatitudes and orientation of rigid
Several generations of mafic dyke swarms of different ages and geochemical characteristics cut Precambrian rocks of the southern part of the Siberian craton(Irkutsk Promontory).Each generation of dykes is related to a
We present a summary of late Paleoproterozoic to Neoproterozoic mafic magmatism in the Siberian craton which allows us distinguish following main pulses of mafic dyke emplacement:1)1860–1850 Ma mafic dykes are locali...We present a summary of late Paleoproterozoic to Neoproterozoic mafic magmatism in the Siberian craton which allows us distinguish following main pulses of mafic dyke emplacement:1)1860–1850 Ma mafic dykes are localized within the展开更多
基金granted by the National Natural Science Foundation of China(Grant Nos.41761144072 and 41888101).
文摘The"Boring Billion"refers the era between c.1.8 and 0.8 billion years ago(Ga)(Holland,2006;Young,2013).Especially,the period from 1.6 to 1.0 Ga is known as"the dullest time in Earth’s deep-time history"(Buick et al.,1995).The reason why this period is referred to as the"Boring Billion"is because there were very few’special’or’interesting’events discovered in the geological or geochemical records over nearly one-fourth of Earth's deep-time history.
基金funded by grant 14-05-00731 from the Russian Foundation of Basic Research
文摘Tectonic evolution and paleogeography of the two major continental blocks Fennoscandia and VolgoSarmatia during their docking to form the East European Craton(Baltica)at 1.8–1.7 Ga represent important‘puzzle
文摘There are only two quantitative tools for Precambrian paleogeographic reconstructions–paleomagnetic data and dyke swarms geometries.Paleomagnetic data provide information about paleolatitudes and orientation of rigid
文摘Several generations of mafic dyke swarms of different ages and geochemical characteristics cut Precambrian rocks of the southern part of the Siberian craton(Irkutsk Promontory).Each generation of dykes is related to a
文摘We present a summary of late Paleoproterozoic to Neoproterozoic mafic magmatism in the Siberian craton which allows us distinguish following main pulses of mafic dyke emplacement:1)1860–1850 Ma mafic dykes are localized within the