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Oil and Gas Potential of Eurasian Western Arctic Shelf/Exploration in the Nearshore Area of Northeastern Baltic Shield

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Open Journal of Geology 2013年第3期3卷 262-271页

作者： Sanghee Shin George V. Chilingar oleg sorokhtin Nikolai O. sorokhtin Geotechnical Engineering Research Division Korea Institute of Construction Technology Goyang City South Korea

A number of large and unique oil and gas fields were discovered over the western Arctic shelf of Eurasia. Some of them were partially appraised. Also, there are three potentially hydrocarbon-rich but insufficiently studied areas in the region. The discovery of commercial accumulations there would substantially increase the petroleum potential of the entire region. These areas are northern Murmansk Oblast, on the Rybachy Peninsula, the Franz-Joseph Land area, and?the North Kara Shelf. It is suggested that oil and gas field discoveries in the former two areas are most expedient under current conditions. The oil and gas potential of the northwestern Kola Peninsula is reviewed in more detail.

关键词： Arctic Shelf Geodynamic Evolution Baltic Shield Oil Potential Gas Potential

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Formation of Glaciation Epochs

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Journal of Environmental Protection 2013年第6期4卷 516-521页

作者： Sanghee Shin George V. Chilingar oleg sorokhtin Nikolai O. sorokhtin Geodynamics and Paleo-Oceanology Laboratory Oceanology Institute Russian Academy of Sciences Moscow Russia Geotechnical Engineering Research Division Korea Institute of Construction Technology Goyang City South Korea Rudolf W. Gunnerman Energy and Environment Laboratory University of Southern California Los Angeles USA Seismology and Geodynamics Laboratory Oceanology Institute Russian Academy of Sciences Moscow Russia

The effect of Earth precession angle on a climate is presented here. It is shown that the glaciation epochs occurred only when the precession angle was low. After the continental glaciation formed in the Northern hemisphere, Earth’s spherecal symmetry was disrupted and its precession angle increased drastically. As a result, a drastic and rapid climate warm-up occurred, the glaciers melted down and an interglacial stadial1 began. Subsequently, affected by the Lunar-Solar gravity pull on the Earth’s equatorial swelling, the precession angle gradually decreased and a new cooling-down phase occurred. As a result, there was nonlinear oscillation of Earth’s climate with periods on the order of 100 - 120 MY.

关键词： Earth’s Precession Glaciation Epochs Climate Evolution Climate Change Global Warming Global Cooling

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