Thèse de doctorat : Université de Fribourg, 2003 ; Nr. 1407.
During the Late Oxfordian and earliest Kimmeridgian, today’s central Swiss Jura Mountains developed as a shallow carbonate-dominated plat form. At the threshold between boreal depositional areas to the north and the Tethys ocean to the south, dynamic sedimentatary systems developed under a subtropical and semiarid to arid climate (palaeolatitude 33°to38°N). Sedimentological analyses of the 6...
|
