Results 181 to 190 of about 207,177 (197)
Some of the next articles are maybe not open access.

Arbuckle Source for Atoka Formation Flysch, Ouachita Mountains Frontal Belt, Oklahoma: New Evidence for Paleocurrents: ERRATUM

AAPG Bulletin, 1988
ABSTRACT In the abstract by Charles A. Ferguson and Neil H. Suneson, entitled “Arbuckle Source for Atoka Formation Flysch, Ouachita Mountains Frontal Belt, Oklahoma: New Evidence for Paleocurrents” (AAPG Bulletin, v. 72, p. 184-185), the final sentence of the second paragraph should read, “The bounding faults would be the southernmost
Charles A. Ferguson, Neil H. Suneson
openaire   +1 more source

Mississippian synorogenic sedimentation in the Variscan belt: Why are NW and SW Iberia flysch basins so different and yet so similar?

2023
Devonian-Carboniferous synorogenic sedimentation is described across the Variscan orogen, as well-preserved exposures in late orogenic structures between continental blocks. Variscan marine sedimentary sequences are described in both colliding continents: Gondwana representative of the southern subducting super-plate, and Laurussia considered as the ...
Ícaro Dias da Silva   +2 more
openaire   +1 more source

Sediment Transport in Headwater Streams of the Carpathian Flysch Belt: Its Nature and Recent Effects of Human Interventions

2015
The paper summarizes results of both empirical and modelling research of bedload transport in headwater streams of the Czech part of the Western Carpathians. Flysch lithology (i.e. alternation of less resistant claystones and sandstones) affects bedload transport parameters in view of relatively fine-sized sediment supply resulting in low flow ...
Tomáš Galia   +2 more
openaire   +1 more source

Structural styles of the External Rif and Flysch Domain (Rif belt, northern Morocco) through thermal maturity and structural data

2020
<p>Located in northern Morocco, the Rif belt represents the western edge of the Maghrebides system. This domain underwent a significant Cenozoic alpine compressional deformation, due to the collision between the North African margin and the south-western margin of the exotic Alboran Domain.
Andrea Schito   +5 more
openaire   +1 more source

Hydromorphological parameters of natural channel behavior in conditions of the Hercynian System and the flysch belt of the Western Carpathians on the territory of the Czech Republic

Geomorphology, 2016
Abstract A fundamental prerequisite for assessing the current ecological status of streams is the establishment of reference conditions for each stream type that serve as a benchmark. The hydromorphological reference conditions reflect the natural channel behavior, which is extremely variable.
Kateřina Kujanová   +2 more
openaire   +1 more source

Thermal maturation patterns in Cambro-Ordovician flysch sediments of the Taconic Belt, Gaspé Peninsula

1981
This item was digitized as part of a project to share McGill's intellectual legacy with the public. If you are the copyright holder or a relative of the copyright holder who is deceased, you may request withdrawal by emailing escholarship.library@mcgill.ca.
openaire   +1 more source

The Resurrection Peninsula Ophiolite, Mélange and Accreted Flysch Belts of Southern Alaska as an Analog for Trench-Forearc Systems in Precambrian Orogens

2004
Publisher Summary The Resurrection Peninsula and Knight Island ophiolitic lavas/dikes exhibit both calcalkaline and tholeiitic geochemistry possibly reflecting fractionation from multiple, compositionally diverse parentalmagmas coupled with variable assimilation of flysch metasedimentary rock.
Timothy M. Kusky   +3 more
openaire   +1 more source

Arbuckle Source for Atoka Formation Flysch, Ouachita Mountains Frontal Belt, Oklahoma: New Evidence from Paleocurrents: ABSTRACT

AAPG Bulletin, 1988
In the abstract by Charles A. Ferguson and Neil H. Suneson, entitled "Arbuckle source for Atoka Formation Flysch, Ouachita Mountains Frontal Belt, Oklahoma: New Evidence for Paleocurrents" (AAPG Bulletin, v. 72, p. 184-185), the final sentence of the second paragraph should read, "The bounding faults would be the southernmost of a series of northward ...
openaire   +1 more source

Some examples of deep-seated landslides in the Flysch Belt of the Western Carpathians

2018
O. Krejčí   +8 more
openaire   +1 more source

Changing heavy mineral associations along the Outer Dinaric Eocene flysch belt: evidence for different structures along the rising Dinarides

2003
The Outer Dinaric coastal belt is dominated by thick Mesozoic to Paleogene platform carbonates, which are followed by Eocene flysch deposits and subsequently by various Eocene to Lower Oligocene clastics. Neogene lacustrine sediments are found only in small patches.
Babić, Ljubomir   +2 more
openaire   +1 more source

Home - About - Disclaimer - Privacy