Palynology and British Purbeck facies

Usk Map Area (NTS 103I/09), Near Terrace, British Columbia: Cross-Sections and Volcanic Facies Interpretation

In the sum mer of 2005, one ge ol o gist and three ge ol ogy stu dents work ing for the Brit ish Co lum bia Geo log i cal Sur vey, along with three Kitselas First Na tion re source tech ni cians, sur veyed the Usk map area, near Ter race, BC (Fig. 1). A ma jor ob jec tive of the pro ject was to iden tify sub di vi sions within the Telkwa For ma tion, a unit that had pre vi ously been un di vide...

Principles and methods for automated palynology.

Pollen grains are microscopic so their identification and quantification has, for decades, depended upon human observers using light microscopes: a labour-intensive approach. Modern improvements in computing and imaging hardware and software now bring automation of pollen analyses within reach. In this paper, we provide the first review in over 15 yr of progress towards automation of the part o...

Palynology as a Tool in Bathymetry

Geology and palynology of the Triassic succession of Bjørnøya

Unspecified DOI: 10.1111/j.1751-8369.1990.tb00382.x Posted at the Zurich Open Repository and Archive, University of Zurich ZORA URL: http://doi.org/10.5167/uzh-112675 Originally published at: Mørk, Atle; Vigran, Jorunn Os; Hochuli, Peter A (1990). Geology and palynology of the Triassic succession of Bjørnøya. Polar Research, 8(2):141-163. DOI: 10.1111/j.1751-8369.1990.tb00382.x Geology and paly...

Facies and Facies Architecture of the IvaniÊ Grad Formation (Upper Pannonian) - Sava Depression, NW Croatia

The Sava depression represents the most southern part of the Pannonian basin (Fig. 1). After the Middle Eocene, a long continental phase started in the area represented by the present depression, during which tectonic movements occurred and a fault network was created along which the basin subsided by extension. The oldest proven sediments belong to the fresh-water Ottnangian deposits which are...