Laurie Reisberg

TL;DR: The Central Atlantic magmatic province (CAMP) consists of basic rocks emplaced as shallow intrusions and erupted in large lava flow fields over a land surface area in excess of 10 million km2 on the supercontinent Pangaea at about 201 Ma as discussed by the authors.

TL;DR: In this article, the authors studied the provenance of Palaeogene fluvio-clastic sedimentary rocks that crop out in central Myanmar, namely the Late Middle Eocene-Early Oligocene Pondaung and Yaw Formations, and found no evidence to support a palaeo Tsangpo-Irrawaddy River, at least during the Late Eocene.

TL;DR: Brenan et al. as mentioned in this paper show that the highly siderophile elements (HSE) show a very pronounced affinity for iron metal, which translates into metal/silicate partition coefficients similar to or higher than 10,000 over large ranges of both pressure and temperature.

TL;DR: In this paper, the authors present new geochemical data (major and trace elements, mineral chemistry and combined Sr-Nd-Pb-Os analyses) on 132 samples, aiming to investigate the mantle source of these rocks and correlate them with magmatism from other areas of the CAMP.

TL;DR: In this paper, the authors investigated the possibility of a PREMA-flavoured mantle plume, enriched by 5-20% recycled crustal material, as a possible source for these tholeiites.