Dictionary of Mathematical Geosciences 2017
DOI: 10.1007/978-3-319-57315-1_16
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“…Depending on the internal mixing processes, the components of a massive overcontact system can either merge or shrink within their Roche-lobes and continue to evolve via the chemically homogeneous evolution pathway (Langer 2012;Marchant et al 2016;. Uncertainties in the evolution of these systems is further exacerbated by the lack of observational constraints: So far only eight overcontact systems are known (Almeida et al 2015;Lorenzo et al 2014Lorenzo et al , 2017Hilditch et al 2005;Howarth et al 2015;Popper 1978;Penny et al 2008).…”
Section: Introductionmentioning
confidence: 99%
“…Depending on the internal mixing processes, the components of a massive overcontact system can either merge or shrink within their Roche-lobes and continue to evolve via the chemically homogeneous evolution pathway (Langer 2012;Marchant et al 2016;. Uncertainties in the evolution of these systems is further exacerbated by the lack of observational constraints: So far only eight overcontact systems are known (Almeida et al 2015;Lorenzo et al 2014Lorenzo et al , 2017Hilditch et al 2005;Howarth et al 2015;Popper 1978;Penny et al 2008).…”
Section: Introductionmentioning
confidence: 99%