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11.
New imagery of ～14 100 km2 of seafloor along a 640 km stretch of the Alaska and Beaufort margins (ABM) in water depths from 250 to 2800 m depicts a repetitive association of glaciogenic bedforms (lineations and iceberg scours), broad erosional bathymetric features and adjacent downslope turbidite gullies. These bedforms have styles, depths and orientations similar to features discovered earlier on the Chukchi Borderland, up to 800 km northwest of the ABM. Lineations occur across the surface of a flattened bathymetric bench interpreted to have formed by an ice shelf sliding along the continental slope and scraping the seafloor at temporary grounding locations. The glacial geology of surrounding areas suggests that an ice shelf probably flowed from the mouths of overdeepened glacial troughs in the Canadian Arctic Archipelago westward along the ABM and across the Chukchi Borderland. This curved pathway indicates an obstruction to ice flow in the central Canada Basin, possibly caused by either a basin‐wide ice shelf or by a pile‐up of mega‐bergs originating from the Eurasian side of the Arctic Ocean. The ice shelf that affected the ABM may have formed between Oxygen Isotopic Stage 4 to 5b, possibly correlating to an inferred intra‐Stage 5 widespread Beringian glaciation. Evidence for glaciogenic features on the ABM corroborates suggestions that large ice volumes and extents existed in the Arctic during Pleistocene glacial periods. These findings have far‐reaching implications for Arctic climate studies, ocean circulation, sediment stratigraphy and the stability of circum‐Arctic continental ice masses. Copyright © 2007 John Wiley & Sons, Ltd. 相似文献
12.
Margo Kleinfeld 《GeoJournal》2005,64(4):287-295
This paper describes the changing discourses of territory in Sri Lanka and their utility in conflict relations. The primordial
homeland has been at the center of Sri Lanka’s armed struggle, in which both Sinhalese and Tamil nationalisms have used claims
of ancient and ethnically determined territories to justify their right to self-determination, territorial sovereignty, and
armed struggle. This identity–territory nexus based on historical argument has been destabilized in Sri Lanka, however. Scholarly
findings suggest that historical linkages between ethnicity and territory in Sri Lanka are highly problematic and are no longer
effectual means for adjudicating territorial desires in Sri Lanka and producing stable homelands. I argue that rights-based
territorial discourses have emerged to enhance the old historical justifications for territorial authority. New narratives
based upon fulfilling or denying human rights have been put to work linking authority to territory based upon moral fitness
and unfitness, political legitimacy and illegitimacy, and ultimately, upon which political actor deserves to rule the territorially
bound population under its control. The first part of the paper examines historical narratives linking national homelands
to identity as well as scholarly work that deconstructs this linkage. In part two, external sovereignty and political legitimacy
are discussed as the starting point for understanding how rights-based discourses justify territorial claims. In part three,
accusations related to human rights violations are described as an important vehicle for shaming political adversaries, undermining
their legitimacy, and making and unmaking territorial claims in Sri Lanka. 相似文献
13.
Paul J. Umhoefer Tobias Schwennicke† Maya T. Del Margo Gabriela Ruiz-Geraldo† James C. Ingle Jr. ‡ William McIntosh§ 《Basin Research》2007,19(2):297-322
Transtensional basins are sparsely described in the literature compared with other basin types. The oblique‐divergent plate boundary in the southern Gulf of California has many transtensional basins: we have studied those on San Jose island and two other transtensional basins in the region. One major type of transtensional basin common in the southern Gulf of California region is a fault‐termination basin formed where normal faults splay off of strike‐slip faults. These basins suggest a model for transtensional fault‐termination basins that includes traits that show a hybrid nature between classic rift and strike‐slip (pull‐apart) basins. The traits include combinations of oblique, strike‐slip and normal faults with common steps and bends, buttress unconformities between the fault steps and beyond the ends of faults, a common facies pattern of terrestrial strata changing upward and away from the faults into marine strata, small fault blocks within the basin that result in complex lateral facies relations, common Gilbert deltas, dramatic termination of the margin of the basin by means of fault reorganization and boundary faults dying and an overall short basin history (few million years). Similar transtensional fault‐termination basins are present in Death Valley and other parts of the Eastern California shear zone of the western United States, northern Aegean Sea and along ancient strike‐slip faults. 相似文献
14.
William H. Orem Calin A. Tatu Harry E. Lerch Cynthia A. Rice Timothy T. Bartos Anne L. Bates Susan Tewalt Margo D. Corum 《Applied Geochemistry》2007
The organic composition of produced water samples from coalbed natural gas (CBNG) wells in the Powder River Basin, WY, sampled in 2001 and 2002 are reported as part of a larger study of the potential health and environmental effects of organic compounds derived from coal. The quality of CBNG produced waters is a potential environmental concern and disposal problem for CBNG producers, and no previous studies of organic compounds in CBNG produced water have been published. Organic compounds identified in the produced water samples included: phenols, biphenyls, N-, O-, and S-containing heterocyclic compounds, polycyclic aromatic hydrocarbons (PAHs), aromatic amines, various non-aromatic compounds, and phthalates. Many of the identified organic compounds (phenols, heterocyclic compounds, PAHs) are probably coal-derived. PAHs represented the group of organic compounds most commonly observed. Concentrations of total PAHs ranged up to 23 μg/L. Concentrations of individual compounds ranged from about 18 to <0.01 μg/L. Temporal variability of organic compound concentrations was documented, as two wells with relatively high organic compound contents in produced water in 2001 had much lower concentrations in 2002. 相似文献
15.
Angela Boley Joris Mergaert Claude Muller Henning Lebrenz Margo C. Cnockaert Wolf‐Rüdiger Müller Jean Swings 《洁净——土壤、空气、水》2003,31(3):195-203
A combination of denitrification and pesticide sorption with the biodegradable polymer poly(?‐caprolactone) (PCL) was examined. The function of PCL is to act as carbon source and carrier for the bacteria and simultaneously as sorbent for the pesticide endosulfan. In a short‐term examination (1 month) the addition of the pesticide endosulfan to a continuous‐flow fixed‐bed reactor resulted in an inhibition of biomass production without reduction of the denitrification performance. However in a long‐term semi‐batch reactor test (6 months) biomass production and partly denitrification rates were affected. No significant differences in microbial composition between the reactors were observed. Regardless of the type of reactor or presence of endosulfan, Acidovorax facilis was the main constituent. 相似文献
16.
Daniel J. Fornari David G. Gallo Margo H. Edwards John A. Madsen Michael R. Perfit Alexander N. Shor 《Marine Geophysical Researches》1989,11(4):263-299
The Siqueiros transform fault system, which offsets the East Pacific Rise between 8°20N–8°30N, has been mapped with the Sea MARC II sonar system and is found to consist of four intra-transform spreading centers and five strike-slip faults. The bathymetric and side-looking sonar data define the total width of the transform domain to be 20km. The transform domain includes prominent topographic features that are related to either seafloor spreading processes at the short spreading centers or shearing along the bounding faults. The spreading axes and the seafloor on the flanks of each small spreading center comprise morphological and structural features which suggest that the two western spreading centers are older than the eastern spreading centers. Structural data for the Clipperton, Orozco and Siqueiros transforms, indicate that the relative plate motion geometry of the Pacific-Cocos plate boundary has been stable for the past 1.5 Ma. Because the seafloor spreading fabric on the flanks of the western spreading centers is 500 000 years old and parallels the present EPR abyssal hill trend (350°) we conclude that a small change in plate motion was not the cause for intra-transform spreading center development in Siqueiros. We suggest that the impetus for the development of intra-transform spreading centers along the Siqueiros transform system was provided by the interaction of small melt anomalies in the mantle (SMAM) with deepseated, throughgoing lithospheric fractures within the shear zone. Initially, eruption sites may have been preferentially located along strike-slip faults and/or along cross-faults that eventually developed into pull-apart basins. Spreading centers C and D in the eastern portion of Siqueiros are in this initial pull-apart stage. Continued intrusion and volcanism along a short ridge within a pull-apart basin may lead to the formation of a stable, small intra-transform spreading center that creates a narrow swath of ridge-parallel structures within the transform domain. The morphology and structure of the axes and flanks of spreading centers A and B in the western and central portion of Siqueiros reflect this type of evolution and suggest that magmatism associated with these intra-transform spreading centers has been active for the past 0.5–1.0 Ma. 相似文献
17.
M. T. Tomczak L. Szymanek M. Pastuszak W. Grygiel M. Zalewski S. Gromisz A. Ameryk J. Kownacka I. Psuty E. Kuzebski R. Grzebielec P. Margoński 《Estuaries and Coasts》2016,39(3):593-604
An integrated trend assessment was conducted for the Gulf of Gdańsk (GoG), Baltic Sea for the period 1994–2010 to describe changes and potentially important drivers of the ecosystem. We found changes in the biota, including an increase in open sea taxa (flatfish, sprat and cod), a decrease in typical coastal species such as eelpout and lumpfish and an increase in primary production. The analyses further suggest that changes in the food web were driven by a combination of anthropogenic pressures (e.g., nutrient loadings and fisheries) and possible interactions with climatic disturbance. Our analyses show that significant changes occurred in the GoG ecosystem between 1994 and 2010. The primary drivers and mechanisms of these changes are discussed. We describe this alteration of the GoG within the context of similar temporal patterns identified in adjacent areas. 相似文献
18.
Amateur decision-making in avalanche terrain with and without a decision aid: a stated choice survey
Avalanches pose a serious threat to recreational backcountry travelers in mountainous terrain. This study explores how the
three main amateur user groups of avalanche terrain in western Canada (backcountry skiers, out-of-bound skiers, and snowmobile
riders) balance recreational goals with safety concerns when choosing backcountry destinations under varying avalanche conditions.
Using a discrete choice experiment (DCE), a stated preference technique, the study first examines the strengths and weaknesses
in the decision process of the three amateur groups by comparing their responses with the choice patterns of professional
mountain guides. The results show that the decision-making strategies employed by the respective amateur groups vary considerably
in their level of complexity and the degree to which avalanche safety considerations are incorporated. Second, we examine
the effects of a decision aid that preprocesses the most crucial pieces of avalanche hazard information on the decision preferences
of the amateur groups in the DCE. The results show that a relatively simple decision aid can influence the decision-making
process considerably and steer users towards more avalanche hazard sensitive behaviour. 相似文献
19.
Xiang Liu Quanwei Li Thomas P. Krichbaum Margo F. Aller Hugh D. Aller 《Astrophysics and Space Science》2013,346(1):15-17
We carried out intra-day variability (IDV) observations from August 2005 to January 2010 with the Urumqi 25 m radio telescope for a dozen IDV sources including the quasar 0917+624. This target exhibited pronounced centimeter-band, intra-day variability during the 1980s–1990s, but its strong IDV phase ceased in 2000. The source showed no IDV in the majority of the Urumqi observing sessions, although weak IDV activity was detected in some. Multifrequency UMRAO data for 0917+624 show that the spectral index is steeper during the weak and non-IDV phases than during the strong IDV phase, supporting the idea that the size of the scintillating component may be enlarged in the weak/non IDV phases. 相似文献