by Bureau of Economic Geology, University of Texas at Austin in Austin, Tex .
Written in English
Includes bibliographical references (p. 44-47).
|Statement||Thomas C. Gustavson.|
|Series||Report of investigations ;, no. 198, Report of investigations (University of Texas at Austin. Bureau of Economic Geology) ;, no. 198.|
|LC Classifications||QE167 .T42 no. 198, QE471 .T42 no. 198|
|The Physical Object|
|Pagination||v, 49 p. :|
|Number of Pages||49|
|LC Control Number||91623555|
Arid Basin Depositional Systems and Paleosols: Fort Hancock and Camp Rice Formations, Hueco Bolson and Adjacent Mexico Abstract The Hueco Bolson is a segment of the Rio Grande Rift that formed as a result of late Tertiary Basin and Range deformation. Book Chapter Deposystems, Paleosols, and Climatic Variability in a Continental System: The Upper Triassic Chinle Formation, Colorado Plateau, U.S.A. Author(s) Russell F. Dubiel Russell F. Dubiel U.S. Geological Survey, MS Box DFC, Denver, Colorado, USA. Terrestrial Depositional Systems: Deciphering Complexities through Multiple Stratigraphic Methods is the first collection of contributed articles that not only introduces young geoscientists to biostratigraphy, chemostratigraphy, magnetostratigraphy, and lithostratigraphy, but also provides seasoned practitioners with a standard reference that showcases the topic’s most recent developments in research and . Overview of the Origin, Depositional Histories, and Petroleum Systems of the Sedimentary Basins of the Eastern United States Author(s) James L. Coleman.
Gustavason TC () Arid basin depositional systems and paleosols: Fort Hancock and Camp Rice Formations (Pliocene-Pleistocene), Hueco Basin, West Texas and adjacent Mexico. Texas Bureau Economic Geology Report Investigations , 49 p Google Scholar. Allard W. Martinius works for Statoil R&D with additional experience from technical service (production and exploration) as well as field development. His main interests are in clastic sedimentology and stratigraphy of fluvial and shallow marine systems, fauna-substrate relationships, and static and dynamic reservoir characterization for hydrocarbon production. ABSTRACT: The Upper Triassic Chinle Formation of the Colorado Plateau in the western United States was deposited as a continental fluvial-floodplainlacustrine- eolian depositional system near the. Identiﬁcation of an anastomosing river system in the Early Cretaceous Khorat Basin, northeastern Thailand, using stratigraphy and paleosols Yu Horiuchia,⇑, Punya Charusirib, Ken-ichiro Hisadac a Geological Survey of Japan, AIST, Higashi, Tsukuba, Ibaraki , Japan bEarthquake and Tectonic Geology Research Unit (EATGRU), c/o Department of Geology, Faculty of Science.
In the Maastrichtian in the Bauru Basin, the paleosols with Bkm are older and more arid environments, and those with Bt were formed in wetter weather, but not enough to lead to the genesis of. Sediments formed in this depositional system are interlayered northeastwards with arid alluvial fans of the Marília Formation, and southwestwards with ephemeral palustrine deposits of the ArF. These formations reach only the initial stages of mesodiagenesis (Fernandes et al., ). Shelf-margin deltas and linked downslope depositional systems are in most cases fed by alluvial valleys that serve to deliver sediment eroded from the hinterland. Accordingly, alluvial valleys provide the link between processes that control sediment flux to the continental margin and processes that control dispersal into the basin. Arid Basin Depositional Systems and Paleosols: Fort Hancock and Camp Rice Formations (Pliocene-Pleistocene), Hueco Bolson, West Texas and Adjacent Mexico, by T. C. Gustavson. 49 p., 29 figs., 3 tables, 1 appendix,