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  • Articles  (141)
  • AERODYNAMICS
  • Geology
  • LUNAR AND PLANETARY EXPLORATION
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Journal
Topic
  • 1
    Electronic Resource
    Electronic Resource
    The relationship between resources and reserves - Estimates for US coal
    Amsterdam : Elsevier
    Resources Policy 8 (1982), S. 53-58 
    Details
    ISSN: 0301-4207
    Keywords: Coal ; Geology ; USA
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Energy, Environment Protection, Nuclear Power Engineering , Economics
    Type of Medium: Electronic Resource
    URL: http://linkinghub.elsevier.com/retrieve/pii/0301-4207(82)90007-1
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  • 2
    Electronic Resource
    Electronic Resource
    Description of the fossiliferous units at Pasalar, Turkey
    Amsterdam : Elsevier
    Journal of Human Evolution 19 (1990), S. 343-361 
    Details
    ISSN: 0047-2484
    Keywords: Geology ; Lithology ; Miocene ; Pasalar ; Turkey
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Biology
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1016/0047-2484(90)90049-H
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  • 3
    Electronic Resource
    Electronic Resource
    A study on geology, geomorphology, hydrology, groundwater, and physical resources of the desertified Badia environment in Jordan towards sustainable development (1996)
    Springer
    Environmental geology 27 (1996), S. 198-209 
    Details
    ISSN: 1432-0495
    Keywords: Geomorphology ; Geology ; Hydrology ; Groundwater ; Physical resources ; Badia ; Arid lands ; Sustainable development ; Natural resources
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract This paper summarizes information on geomorphology and physical resources as a part of the Jordan Badia Research and Development Program. The research focused on the issue of the environment in arid lands as an aid to providing practical options for sustainable development, for the benefit not only of the Hashemite Kingdom of Jordan but of other arid regions of the world. The research is significant in that there is a need to identify usable natural resources and establish a framework for their effective exploitation and management in a marginal, fragile environment, which is sensitive to change. Pressure for development of the Badia stems from the fact that the great majority of the population in Jordan is compressed into less than 10% of the country by environmental constraints. It is hoped that the Jordan Badia Research and Development Program will provide the required framework to ease current environmental pressures, encourage migration to the Badia, a sparsely populated region, and establish economically and ecologically self-supporting communities. This paper discusses the following areas that are related to the sustainable development of the Jordan Badia with special emphasis on the Safawi area in the northern Jordan Badia; geomorphology, including landform, processes, and hazards; geology and physical resources; hydrology; surface water and water engineering; and groundwater.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00770433
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  • 4
    Electronic Resource
    Electronic Resource
    Hydrogeology and geochemistry in the Curuksu (Denizli) hydrothermal field, western Turkey (2000)
    Springer
    Environmental geology 39 (2000), S. 1169-1180 
    Details
    ISSN: 1432-0495
    Keywords: Key words Geochemistry ; Geology ; Hydrogeology ; Hydrothermal waters ; Isotopes
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract  Curuksu is a low temperature hydrothermal system located within the upper sector of the B. Menderes Graben. The hydrologic structure of the Curuksu hydrothermal system is largely controlled by major graben faults where it is characterized by the presence of two thermal reservoirs. One is formed by Paleozoic quartzite, schist and marble units, and the second consists of Pliocene limestone-travertine units. The thermal conditions in the Curuksu region indicate that the regional tectonics and resulting local stress field control low temperatures activity. Temperatures of 30 springs emerging in the study area range between 15 and 55  °C. These springs are classified as cold fresh, warm mineral and thermal waters. Pamukkale, Karahayıt and Honaz springs are steam condensate waters, whereas Curuksu springs are commonly steam-heated waters with respect to the major anion concentrations. The reservoir temperatures have been estimated from chemical compositions by utilizing simultaneously, geothermometers and mixing models. According to these thermometric methods, the most probable subsurface temperature is in the range of 62–90  °C. However, the mixing models suggest a temperature level of 80  °C for the parent water. The system has low total dissolved solid (TDS) of ∼1000–1500 mg/l, which indicate that these waters undergo conductive cooling within the reservoir.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/s002540000139
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  • 5
    Electronic Resource
    Electronic Resource
    Two tools for integrating geology into ecosystem studies (1995)
    Springer
    Environmental geology 26 (1995), S. 246-251 
    Details
    ISSN: 1432-0495
    Keywords: Ecosystem ; Land management ; Matrix ; Hierarachy ; Geology
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Increased interest in understanding ecosystems as a basis for land management requires new approaches for incorporating geology into the process. Limited work performed by geologists to ensure adequate information about geologic interrelationships with the biosphere is available to land managers and other earth scientists. This paper proposes two processes that will aid in increasing the amount and quality of geologic information available to land managers and other earth scientists. First, the geologic integration with ecosystem matrix is a computer data-base format presenting the chemical and physical interrelationships of geology with the biosphere. Second, the geologic terrane land unit hierarchy is an approach to segregating the earth's surface into a hierarchy of land units to simplify applying data-base information to the land.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00770475
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  • 6
    Electronic Resource
    Electronic Resource
    A study on geology, geomorphology, hydrology, groundwater, and physical resources of the desertified Badia environment in Jordan towards sustainable development (1996)
    Springer
    Environmental geology 27 (1996), S. 198-209 
    Details
    ISSN: 1432-0495
    Keywords: Key words: Geomorphology ; Geology ; Hydrology ; Groundwater ; Physical resources ; Badia ; Arid lands ; Sustainable development ; Natural resources
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract This paper summarizes information on geomorphology and physical resources as a part of the Jordan Badia Research and Development Program. The research focused on the issue of the environment in arid lands as an aid to providing practical options for sustainable development, for the benefit not only of the Hashemite Kingdom of Jordan but of other arid regions of the world. The research is significant in that there is a need to identify usable natural resources and establish a framework for their effective exploitation and management in a marginal, fragile environment, which is sensitive to change. Pressure for development of the Badia stems from the fact that the great majority of the population in Jordan is compressed into less than 10% of the country by environmental constraints. It is hoped that the Jordan Badia Research and Development Program will provide the required framework to ease current environmental pressures, encourage migration to the Badia, a sparsely populated region, and establish economically and ecologically self-supporting communities. This paper discusses the following areas that are related to the sustainable development of the Jordan Badia with special emphasis on the Safawi area in the northern Jordan Badia; geomorphology, including landform, processes, and hazards; geology and physical resources; hydrology; surface water and water engineering; and groundwater.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00770433
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  • 7
    Electronic Resource
    Electronic Resource
    Modeling wetland loss in coastal Louisiana: Geology, geography, and human modifications (1988)
    Springer
    Environmental management 12 (1988), S. 827-838 
    Details
    ISSN: 1432-1009
    Keywords: Wetland loss ; Geology ; Coast ; Models ; Louisiana
    Source: Springer Online Journal Archives 1860-2000
    Topics: Energy, Environment Protection, Nuclear Power Engineering
    Notes: Abstract Habitat change in coastal Louisiana from 1955/6 to 1978 was analyzed to determine the influence of geological and man-made changes on landscape patterns within 7.5 min quadrangle maps. Three quantitative analyses were used: principal components anlaysis, multiple regression analysis, and cluster analysis. Regional differences in land loss rates reflect variations in geology and the deltaic growth/decay cycles, man-induced chages in hydrology (principally canal dredging and spoil banking), and land-use changes (principally urbanization and agricultural expansion). The coastal zone is not homogeneous with respect to these variables and the interaction between causal factors leading to wetland loss is therefore locally variable and complex. The relationship between wetland loss, hydrologic changes, and geology can be described with statistically meaningful results, even though these data are insufficient to precisely quantify the relationship. However, these data support the hypothesis that the indirect impacts of man-induced changes (hydrologic and land use) may be as influential as the direct impacts resulting in converting wetlands to open water (canals) or modified (impounded) habitat. Three regions within the Louisiana coastal zone can be defined, based on the potential causal factors used in the analyses. The moderate (mean = 22%) wetland loss rates in region 1 are a result of relatively high canal density and developed area in marshes which overlie sediments of moderate age and depth; local geology acts, in this case, to lessen indirect impacts. On the other hand, wetland loss rates in region 2 are high (mean = 36%), despite fewer man-induced impacts; the potential for increased wetland loss due to both direct and indirect effects of man's activity in these areas is high. Conversely, wetland loss (mean = 20%) in region 3 is apparently least influenced by man's activity in the coastal zone because of sedimentary geology (old, thin sediments), even though these areas have already experienced significant direct habitat alteration and wetland loss.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF01867610
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  • 8
    Electronic Resource
    Electronic Resource
    Relationships between stream water chemistry and catchment geology in a mountainous region in Nagano Prefecture, Japan II: mid to southern part along the Median Tectonic Line (2000)
    Springer
    Limnology 1 (2000), S. 117-127 
    Details
    ISSN: 1439-863X
    Keywords: Key words Major ions ; Stream waters ; Water-rock interaction ; Geology ; Mapping ; Median Tectonic Line ; Nagano Prefecture
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Major ion concentrations were determined for a large number of stream water samples collected from the mountainous area around the Median Tectonic Line (MTL) in the mid to southern part of Nagano Prefecture, Japan. The MTL, a major fault in the accretionary sedimentary complex to Japan Arc, extending linearly in the east–west direction in southwest Japan, bends in this area to south–north along the Akaishi Mountain chain. To the east of the MTL are, in order, Jurassic metamorphic rocks, including black/green schists and ultra-basic serpentinite (Sambagawa-Mikabu Belt); Jurassic mudstone with voluminous chert and calcite (Chichibu Belt); and Cretaceous sandstone (Shimanto Belt). On the other hand, on the west side of the MTL, Cretaceous granitic rocks (including tonalite and quartzdiorite) intruded and significantly metamorphosed the Jurassic sedimentary systems (Ryoke-Belt). In this area, more than 200 water samples were collected from small streams. Ion concentrations were analyzed by ion chromatography, whereby higher ion concentrations relatively rich in Mg2+ and Ca2+ and lower concentrations relatively rich in Na+ were obvious for the streams in Sambagawa-Mikabu, Chichibu, and Ryoke Belts, respectively. These tendencies could be explained by whole rock analysis on XRF (X-ray fluorescence spectrometry) as well as by a preliminary leaching experiment of the powdered rock samples with water. The results strongly suggested that the analytical data of the major ions in the stream waters might be compiled into a hydrogeochemical map, corresponding to the geological map.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/s102010070017
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  • 9
    Electronic Resource
    Electronic Resource
    Classifying mineral potential in support of land-use policy decisions in British Columbia, Canada (1992)
    Springer
    Natural resources research 1 (1992), S. 85-96 
    Details
    ISSN: 1573-8981
    Keywords: Mineral potential ; Land use ; British Columbia ; Geology ; Geochemistry ; Mineral deposits
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract British Columbia covers a vast segment of the Cordillera Mountain system that is richly endowed with a diversity of resources. British Columbia's historic patterns of resource development increasingly have been in conflict with demands for greater environmental protection. To avoid such conflicts, a recently legislated process that provides for detailed mineral resource assessments in candidate park areas has stimulated the creation of a mineral potential classification system for use in land-use planning and policy decisions. A mineral potential study of the Chilko Lake Planning Area provided three unique categories of field data on which to build the classification system. These categories are geological setting, geochemistry, and mineral occurrences. Data in each category were compiled independently to provide indicators of mineral potential. The field data were used to develop a widely understood classification of mineral potential. The classification is based on two factors: favorability and degree of confidence. Favorability refers to how field data satisfy criteria for established mineral deposit models. A greater degree of confidence in the mineral potential rating is achieved as more data categories are determined to be favorable. A mineral potential map shows the classification ratings. The classification conveys to land-use planners all the concepts necessary to appreciate mineral potential designations. It is used to produce a concise map highlighting zones worthy of exploration by industry. The interpretive display maintains broad appeal, but by adapting data to a geographic information system, more detailed interpretations are possible. Geophysical data can also be accom-modated by expanding the system. Qualitative descriptions of each mineral potential category describe the likelihood for future exploration activities as a measure of expected land use. The relation between resource values and land-use activities has been confirmed by industry follow-up in the area.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF01782115
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  • 10
    Electronic Resource
    Electronic Resource
    Computerized vision for the geologist (1983)
    Springer
    Mathematical geology 15 (1983), S. 3-23 
    Details
    ISSN: 1573-8868
    Keywords: Geology ; petrology ; geological maps ; geological surveys ; image analysis ; image processing ; binary images ; component labels ; phase labels ; erosion ; dilatation ; logical operations ; spatial operations ; GIAPP ; Prospector ; CHARAN ; SIMSAG
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Mathematics
    Notes: Abstract The digital computer can be a tireless friend and assistant to the geologist. The computer has no innate intelligence, but given adequate programs to analyze and interrelate the information on maps, photos, surveys, and other material, the computer can serve as an analytical tool and consultant. To the geologist's qualitative knowledge, theories, and models can be added the possibility of the computer's mathematically precise numerical answers, confirming or refuting the original ideas. In the interactive mode in particular, a dialogue between the geologist and the computer is established, where the geologist and the computer can complement each other's abilities. The basic principles of processing two-dimensional geological data, such as maps, charts, photos, and survey results, are discussed. Some comparisons are also made between the rule-based methods of Prospector, developed at Stanford Research Institute, and the more intuitively guided image-based procedures of GIAPP, developed on the equipment at the National Research Council of Canada, in collaboration with the Geological Survey of Canada and the University of Ottawa.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF01030073
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