Results 121 to 130 of about 25,106,784 (215)
1-Introduction: Kopeh-Dagh sedimentary basin is located in NE of Iran and is mainly composed of Mesozoic and Cenozoic sedimentary rocks (35 30ˊ-38 15ˊ N, 54 00-61 31ˊE)(Afshar-Harb 1994).
Mohsen Allameh +2 more
doaj
Vegetation climate and marine environmental reconstruction in the western Mediterranean (southern Rifian corridor, Morocco) over the Tortonian-Messinian transition. [PDF]
Targhi S +5 more
europepmc +1 more source
La matière organique sédimentaire des formations argileuses du Kimméridgien–Tithonien du Boulonnais a été étudiée sous un aspect multidisciplinaire : pétrographique, géochimique et granulométrique, ainsi que du point de vue de la stratigraphie ...
Bialkowski, Anne +3 more
core +3 more sources
In the deep-water area of the Zhu Ⅱ Depression of the Pearl River Mouth Basin, the Baiyun Sag develops three types of source rocks: mudstone, carbonaceous mudstone, and coal.
Yue CHEN +5 more
doaj +1 more source
Problems Statement and Purpose. The work is relevant because of the need to create a reliable history of the formation of the physical and geographical environment of the Paleogene in the territory of Zhytomyr Polissya to decipher the processes of amber ...
Тетяна Шевченко +3 more
doaj +1 more source
Vegetation and climate change at the southern margin of the Neo-Tethys during the Cenomanian (Late Cretaceous): Evidence from Egypt. [PDF]
El Atfy H +3 more
europepmc +1 more source
Variação isotópicas d13C carbonatos na Sucessão da Baía de Três Angras: afloramento Mesozóico da Carrapateira (Kimeridgiano Inferior) [PDF]
O afloramento Mesozóico da Carrapateira (AMC), localizado a 20 km a norte de Sagres é formado por sedimentos do Triássico Superior ao Kimmeridgiano.
Borges, Marisa +5 more
core
Non-vital staining, especially with rose Bengal, has been widely used in ecological studies to differentiate between the tests of dead(unstained) foraminifera from those presumed to be living at the time of collection (stained).
Bowser, S.S., Murray, J.W.
core
A dél-dunántúli középső triász karbonátos kőzetek ciklus-sztratigráfiai vizsgálata = Cyclostratigraphic analysis of Southern Hungarian middle triassic carbonates [PDF]
A ciklus-sztatigráfiai elemzések alapján a délkelet-dunántúl középső triász karbonátok három harmadrendű, aszimmetrikus üledékciklust képviselnek. Ezek közül két teljes ciklus az anizuszi emelethez köthető.
Konrád, Gyula, Török, Ákos
core
Greenhouse conditions in lower Eocene coastal wetlands?-Lessons from Schöningen, Northern Germany. [PDF]
Lenz OK, Riegel W, Wilde V.
europepmc +1 more source

