In this section
@article{Evans:2018:10.1139/cjes-2018-0081,
author = {Evans, ME and Muxworthy, AR},
doi = {10.1139/cjes-2018-0081},
journal = {Canadian Journal of Earth Sciences},
pages = {912--916},
title = {Vaalbara Palaeomagnetism},
url = {http://dx.doi.org/10.1139/cjes-2018-0081},
volume = {56},
year = {2018}
}
TY - JOUR
AB - Vaalbara is the name given to a proposed configuration of continental blocks—the Kaapvaal craton (southern Africa) and the Pilbara craton (north-western Australia)—thought to be the Earth’s oldest supercraton assemblage. Its temporal history is poorly defined, but it has been suggested that it was stable for at least 400 million years, between 3.1 and 2.7 Ga. Here, we present an updated analysis that shows that the existence of a single supercraton between ∼2.9 and ∼2.7 Ga is inconsistent with the available palaeomagnetic data.
AU - Evans,ME
AU - Muxworthy,AR
DO - 10.1139/cjes-2018-0081
EP - 916
PY - 2018///
SN - 0008-4077
SP - 912
TI - Vaalbara Palaeomagnetism
T2 - Canadian Journal of Earth Sciences
UR - http://dx.doi.org/10.1139/cjes-2018-0081
UR - https://www.nrcresearchpress.com/doi/10.1139/cjes-2018-0081#.XZyLIFVKiUk
UR - http://hdl.handle.net/10044/1/62844
VL - 56
ER -