WATER-ROCK INTERACTION PROCESSES IN THE TRIASSIC SANDSTONE AND THE GRANITIC BASEMENT OF THE RHINE GRABEN - GEOCHEMICAL INVESTIGATION OF A GEOTHERMAL RESERVOIR

Saline fluids have been collected in the Rhine Graben over the last tw o decades. both from the Triassic sandstone aquifer and the granitic b asement down to a depth of 3500m. Their salinities and location are co mpared in order to distinguish the respective influences of temperatur e and host-rock mineralogy in the water-rock interaction processes. Th e comparison shows that sulphates in the sedimentary formations were d issolved by the fluids, which also led to Br enrichment. Mica dissolut ion has strongly increased the Rb and Ca contents, which then provide an indication of the degree of water-rock interaction. The Sr isotopic ratios are used to compare the fluids with the granite minerals. Two relationships are revealed for the fluids in the sandstone and the gra nite, one related to widespread mica dissolution, which could have aff ected both the Buntsandstein and the granite, and the other to subsequ ent plagioclase dissolution, which is observed only in the granite. Co mputations showed that 12.5g of mica and 1.65g of plagioclase per lite r of fluid have been dissolved. The nature of these two relationships suggests two different evolutions for the fluids and the individualiza tion of the two reservoirs during the graben's history. The cation con centrations are mainly controlled by temperature, and are independent of the type of host rock. Equilibrium with the rock mainly caused Ca a nd K concentration variations, which has induced clear Ca-K and Ca-del ta(18)O, K-delta(18)O correlations. Geothermometric computations indic ate that with increasing depth, the cations, the silica and the delta( 18)O (SO4) geothermometers evolve towards a value close to 230 degrees C. This demonstrates the existence of a hot reservoir in the granite of the graben, at a depth estimated at 4.5-5 km. Copyright (C) 1997 El sevier Science Ltd.