Special Issue "Sedimentary Basins and Orogenic Belts"
A special issue of Geosciences (ISSN 2076-3263).
Deadline for manuscript submissions: closed (30 April 2013)
Prof. Dr. James Schmitt
Department of Earth Sciences, Montana State University, P.O. Box 173480, Bozeman, MT 59717-3480, USA
Interests: relations between deformation and sedimentation; sedimentary basin development; controls on sediment provenance; siliciclastic diagenesis; depositional systems; geoscience education; taphonomy and fossil preservation
The major objective of this special issue of Geosciences is to examine the dynamically linked relations between sedimentary basin and orogenic belt development. Because sedimentary basins serve as the repositories of detritus delivered from deforming and eroding orogens, they record the geodynamic signature of mountain belt development. This sediment source (orogen) to sink (basin) relationship results in a wide spectrum of attributes typically recorded in basin-fill including: (1) tectonic style of lithosphere/crust deformation during orogensis, (2) sedimentary and geomorphic responses to land surface deformation, (3) controls on sediment provenance and dispersal, (4) development of paleotopography, (5) rates and mechanisms of mountain belt uplift and exhumation, (6) distribution and evolution of depositional systems, (7) paleoenvironments and climate and (8) biogeographic parameters.
Specifically, this special issue aims to provide an outlet for rapid, widely accessible publication of peer-reviewed studies utilizing the synorogenic sedimentary basin record to improve understanding of orogenesis in associated mountain belts using both modern and ancient examples from all types of tectonic settings. Research spanning the spectrum of methods ranging from use of more traditional field-based stratigraphic analysis and structural mapping to geochemical and isotopic provenance/subsidence history analysis to basin/orogen modeling approaches is welcome
Prof. Dr. James Schmitt
Manuscripts should be submitted online at www.mdpi.com by registering and logging in to this website. Once you are registered, click here to go to the submission form. Manuscripts can be submitted until the deadline. Papers will be published continuously (as soon as accepted) and will be listed together on the special issue website. Research articles, review articles as well as communications are invited. For planned papers, a title and short abstract (about 100 words) can be sent to the Editorial Office for announcement on this website.
Submitted manuscripts should not have been published previously, nor be under consideration for publication elsewhere (except conference proceedings papers). All manuscripts are refereed through a peer-review process. A guide for authors and other relevant information for submission of manuscripts is available on the Instructions for Authors page. Geosciences is an international peer-reviewed Open Access quarterly journal published by MDPI.
Please visit the Instructions for Authors page before submitting a manuscript. For the first couple of issues the Article Processing Charge (APC) will be waived for well-prepared manuscripts. English correction and/or formatting fees of 250 CHF (Swiss Francs) will be charged in certain cases for those articles accepted for publication that require extensive additional formatting and/or English corrections.
- synorogenic sedimentation
- provenance studies
- sediment dispersal
- uplift and exhumation
- orogens and climate
- subsidence histories and mechanisms
- basin tectonics
- tectonic geomorphology
Article: The Role of Regional and Local Structure in a Late Ordovician (Edenian) Foreland Platform-to-Basin Succession Inboard of the Taconic Orogen, Central Canada
Geosciences 2013, 3(2), 216-239; doi:10.3390/geosciences3020216
Received: 15 March 2013; in revised form: 26 April 2013 / Accepted: 9 May 2013 / Published: 21 May 2013| Download PDF Full-text (8219 KB) | Download XML Full-text
Geosciences 2013, 3(2), 311-330; doi:10.3390/geosciences3020311
Received: 23 March 2013; in revised form: 29 April 2013 / Accepted: 13 May 2013 / Published: 4 June 2013| Download PDF Full-text (27194 KB) | Download XML Full-text
Geosciences 2013, 3(2), 331-353; doi:10.3390/geosciences3020331
Received: 23 March 2013; in revised form: 29 April 2013 / Accepted: 13 May 2013 / Published: 4 June 2013| Download PDF Full-text (19063 KB) | Download XML Full-text
Review: Volcanosedimentary Basins in the Arabian-Nubian Shield: Markers of Repeated Exhumation and Denudation in a Neoproterozoic Accretionary Orogen
Geosciences 2013, 3(3), 389-445; doi:10.3390/geosciences3030389
Received: 7 May 2013; in revised form: 17 June 2013 / Accepted: 19 June 2013 / Published: 9 July 2013| Download PDF Full-text (26910 KB) | Download XML Full-text
Article: Lower Paleogene Tectonostratigraphy of Balochistan: Evidence for Time-Transgressive Late Paleocene-Early Eocene Uplift
Geosciences 2013, 3(3), 466-501; doi:10.3390/geosciences3030466
Received: 1 June 2013; in revised form: 19 July 2013 / Accepted: 19 July 2013 / Published: 29 July 2013| Download PDF Full-text (4004 KB) | Download XML Full-text | Supplementary Files
Geosciences 2013, 3(3), 502-527; doi:10.3390/geosciences3030502
Received: 4 May 2013; in revised form: 11 July 2013 / Accepted: 15 July 2013 / Published: 29 July 2013| Download PDF Full-text (3374 KB) | Download XML Full-text | Supplementary Files
Article: Detrital Zircon Fission-Track Thermochronology of the Present-Day Isère River Drainage System in the Western Alps: No Evidence for Increasing Erosion Rates at 5 Ma
Geosciences 2013, 3(3), 528-542; doi:10.3390/geosciences3030528
Received: 7 May 2013; in revised form: 19 July 2013 / Accepted: 23 July 2013 / Published: 6 August 2013| Download PDF Full-text (2207 KB) | Download XML Full-text
Last update: 13 August 2012