Výsledky vyhledávání - "Susan Bartsch-Winkler"

Summary of the mineral- and energy-resource endowment, BLM roswell resource area, east-central New Mexico

Autor: M. M. Ball, R. F. Kness, J. T. Dutchover, David M. Sutphin, S. L. Korzeb, Susan Bartsch-Winkler

Publikováno v: Nonrenewable Resources. 2:262-283

In this summary of two comprehensive resource reports produced by the U.S. Bureau of Mines and the U.S. Geological Survey for the U.S. Bureau of Land Management, we discuss the mineral- and energyresource endowment of the 14-millon-acre Roswell Resou

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::72afac1c7fe87573e64cf62470324af4
https://doi.org/10.1007/bf02257538

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Utility of radiocarbon-dated stratigraphy in determining late Holocene earthquake recurrence intervals, upper Cook Inlet region, Alaska

Autor: Henry R. Schmoll, Susan Bartsch-Winkler

Publikováno v: Geological Society of America Bulletin. 104:684-694

During the great 1964 earthquake, parts of coastal southern Alaska subsided tectonically as much as 2 m, and this led to burial of high-intertidal organic-rich marshes by low-intertidal and tidal silt. In the tectonically active part of upper Cook In

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::1903dffa1081f12771f6c9c1a8f7d4f2
https://doi.org/10.1130/0016-7606(1992)104<0684:uordsi>2.3.co

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Cycle of earthquake-induced aggradation and related tidal channel shifting, upper Turnagain Arm, Alaska, USA

Autor: Susan Bartsch-Winkler

Publikováno v: Sedimentology. 35:621-628

Aggradation of intertidal sediment in upper Turnagain Arm, a macrotidal estuary located in southern Alaska near Anchorage, began because of subsidence caused by sediment consolidation and tectonic lowering of the land during the earthquake of March 2

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::fa69f6136c515f0286350c7db9a54164
https://doi.org/10.1111/j.1365-3091.1988.tb01240.x

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Holocene history of the estuarine area surrounding Portage, Alaska as recorded in a 93 m core

Autor: Reuben Kachadoorian, Susan Bartsch-Winkler, A. Thomas Ovenshine

Publikováno v: Canadian Journal of Earth Sciences. 20:802-820

A 93 m core obtained at Portage, Alaska records four prograding cycles of estuarine deposition for the past 8230 ± 100 years. Analyses of texture, mineralogy, paleontology, and sedimentary structures enable definition of eight lithologic units. Mine

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::9af731b55aef80e85b66e61f8351edce
https://doi.org/10.1139/e83-071

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Macrotidal Subarctic Environment of Turnagain and Knik Arms, Upper Cook Inlet, Alaska: Sedimentology of the Intertidal Zone

Autor: Susan Bartsch-Winkler, A. Thomas Ovenshine

Publikováno v: SEPM Journal of Sedimentary Research. 54

An extensive sheet of silty sand crossed by tidal channels is exposed at low tide in Turnagain and Knik Arms, Alaska. Transportation and deposition of sediment composing this sheet is the result of strong tidal currents due to the maximum spring tida

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::89d9a9b084012ecedddef9fce9ddadcb
https://doi.org/10.1306/212f85a8-2b24-11d7-8648000102c1865d

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PORTAGE, ALASKA: CASE HISTORY OF AN EARTHQUAKE'S IMPACT ON AN ESTUARINE SYSTEM

Autor: Susan Bartsch-Winkler, A.T. Ovenshine

Regional tectonic subsidence and differential sediment consolidation during the 1964 Alaska earthquake (Richter mag.=8.5) lowered the Portage area into the intertidal zone of Turnagain Arm, forcing abandonment of the town of Portage. Ground subsidenc

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::9208e5a6f316984340fc56eecf8af23f
https://doi.org/10.1016/b978-0-12-751850-3.50023-6

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Bedding Types in Holocene Tidal Channel Sequences, Knik Arm, Upper Cook Inlet, Alaska

Autor: Henry R. Schmoll, Susan Bartsch-Winkler

Publikováno v: SEPM Journal of Sedimentary Research. 54

Uplifted convoluted and horizontal to subhorizontal beds of varying thickness in intertidal silt as old as 3,280 ± 90 yr B.P. are exposed in the banks of tidal channels of unknown depth in the intertidal zone in Knik Arm of Upper Cook Inlet. Interna

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::a024c1cb6d7e0f2c77e3b705314af134
https://doi.org/10.1306/212f85ad-2b24-11d7-8648000102c1865d

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