Lacustrine carbonates accumulate in all climates and in any tectonic situation. Their
depositional patterns are assessed through a database involving literature representing …

Carbonate sediments hold a critical component of the continental sedimentary record on
earth. Carbonates precipitate under all climatic conditions on earth, from arctic to humid …

This text, written by a leading researcher in the field, describes the origin and formation of
lakes in order to give context to the question of how lacustrine deposits form. It explains the …

The post-flysch (Oligocene–Miocene) palaeogeographic evolution of the entire North Alpine
Foreland Basin (NAFB) between Savoy (France) and Lower Austria is presented in eight …

ABSTRACT The Lower Freshwater Molasse (Untere Susswasser Molasse) crops out over a
wide area of the Swiss Molasse Basin. Coarse grained alluvial fan conglomerates dominate …

We present a general stratigraphic synthesis for the Upper Rhine Graben (URG) and the
Swiss Molasse Basin (SMB) from Eocene to Pliocene times. The stratigraphic data were …

During deposition of the Upper Jurassic Morrison Formation, water that originated as
precipitation in uplands to the west of the Western Interior depositional basin infiltrated …

Lacustrine deposits form most of the sedimentary record accumulated throughout the
Miocene in the northern part of the Teruel Graben, a landlocked basin situated in NE Spain …

Purbeckian (lowermost Cretaceous) peritidal carbonates are characterized by open marine,
lagoonal, intertidal and lacustrine facies arranged in Milankovitch‐type shallowing upward …

The formation of carbonate sediments in continental environments is subject to numerous
environmental controls, of which climate is one of the foremost. Consequently, calcareous …