Sediments of MIS 5e age suggested by new OSL dates from the Skilvika section, west Svalbard

Sedimentary facies are assigned to each depositional environment as defined within the Cook Formation with an assumption of some uncertainty degree in interpretation. As seen from

The lack of coarse sediments in the Wood Bay Formation first suggested that no structure existed at the surface along the line of the Billefjorden Fault Zone in Lower Devonian times,

That I goes is indeed used as a multi-turn quotative is suggested by the fact that the average number of presented turns in the sample is 3.4.. Although in a number of contexts only

As expected, heating an unconfined shale sample (experiments 1, 2 and 3) resulted in the formation of more fractures than heating the confined shale sample (experiment 4)

New funds (6) consist of funds that started operating at some point during our sample period and initial funds (7) includes funds that was alive at the beginning of our

Specimens from the block sample that were subjected to simulated tube sample disturbance showed similar stress-strain behavior to that from conventional anisotropically

Our interpretation is that the logged section of Entrada Formation can be described as the damage zone of Little Grand Wash fault and that the sub-vertical fractures define a fracture

(2003) suggested that the rifting that occurred in Cretaceous times can be characterized by (1) formation of large scale normal faults during the early rift phase at about