Late-glacial varved clays in the Bornholm Basin and Hanö Bay

Distribution, thickness, lithology and stratigraphy of varved clays are discussed. The sediments were deposited in the Baltic Ice Lake during the Late Weichselian.     

Deglaciation of the Bara Basin near Malmö, Sweden

Results obtained by mapping and special varved clay investigation show that the so-called Northeastern ice advance (13,500 B.P.) and the Low Baltic readvance (13,000–13,200 B.P.) are separated by a significant deglaciation phase, for which we propose 'Lockarp Interstadial' (13,200-13,500 B.P.) as a time-stratigraphic term to be used in the type area of southwestern Scania.     

Fluid Evolution during HP and UHP Metamorphism in Dabie Shan, China: Constraints from Mineral Chemistry, Fluid Inclusions and Stable Isotopes

The Dabie Shan ultrahigh-pressure (UHP) metamorphic terraneis located in the eastern part of the east–west-strikingQinling–Dabie orogenic belt in China. A major mylonitizedcontact zone of 200–300 m width divides Dabie Shan intothe South Dabie Terrane (SDT) and the North Dabie Complex (NDC).Combined investigation of major and trace element geochemistry,fluid inclusions, and oxygen and hydrogen isotopes constrainsthe fluid history during the metamorphic evolution of the twometamorphic belts, which differ in their fluid and metamorphicevolution. Fluid inclusions in rocks from the SDT are mainlyaqueous with varying salinities, whereas those from the NDCare dominated by CO₂. Low