Veins in the combusted metamorphic rocks, Israel; Weathering or a retrograde event?

For about four decades the Hatrurim Formation (Israel, the Palestinian Authority) and its equivalent in Jordan were considered to have formed between 16 and 3 Ma ago by combustion of bituminous chalks, dehydration and decarbonation, resulting in two stages: a prograde country rock of High-T, Low-P (Portland Cement-like) assemblages, and a retrograde, closely time-related stage, of concrete-like vein fillings of rehydration and recarbonation. dated carbonate (calcite, aragonite, vaterite) containing veins in both spurrite marbles and gehlenite metamorphic rocks by 230Th–234U dating. The ages of most veins range between 250 ka and 30 ka, with only a minority being older than 450 ka (the method limit). δ18O of the vein carbonates indicates water-δ18O as low as − 14‰ (SMOW), much lighter than present-day rain in the area. These values are in accord with previous information on the areaʹs paleo-rain derived from speleothem analysis and from fossil aquifers. Both δ13C (− 18‰ to − 5‰) and 87Sr/86Sr (0.70786–0.70811) ratios indicate interaction between rain-derived circulating solutions and country metamorphic rock-affected water. Thus vein formation is closer to a weathering process rather than to retrograde metamorphism. Textural relationships between vein-filling minerals suggest the possibility that they represent reactivation and replacement of a pre-existing phase by younger minerals. ins, some of them enriched in Cr and Fe bearing minerals, indicate short-distance metal mobilization in the weathering process, as opposed to a large scale nearly closed system behavior in the prograde stage. The occurrence of high-pH waters in the Hatrurim outcrop of north Jordan suggests vein formation in an alkaline environment.