Buchbesprechungen     

F. Steinhauser  W. Mörikofer  J. Drimmel  Peter Steinhauser 《Meteorology and Atmospheric Physics》1965,15(2):251-264

Ohne Zusammenfassung  相似文献   

THE ATLANTIC CITY ORE MINE: A STUDY IN ECONOMIC GEOGRAPHY     

Peter F. Mason 《The Professional geographer》1966,18(5):280-282

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GEOGRAPHIC NOTEBOOK: POLYNESIAN MIGRATION: THE NEW WAVE     

Peter  Pirie 《New Zealand geographer》1966,22(2):182-185

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GEOGRAPHIC NOTEBOOK: THE TURN-ROUND OF SHIPPING IN NEW ZEALAND SAVING THE SECOND MILLION     

Peter J.  Rimmer 《New Zealand geographer》1966,22(1):94-95

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Basalt from Louisiana continental shelf     

Richard Rezak  Thomas T. Tieh 《Geo-Marine Letters》1984,4(2):69-76

A basalt outcrop was discovered on Alderdice Bank on the outer Louisiana continental shelf. The basalt shows an age of 76.8 ± 3.3 × 10⁶ years. Textural, mineralogical, and chemical characteristics indicate that it is an alkali basalt of shallow intrusive origin. It was probably brought to the seafloor by salt tectonics and exposed due to salt dissolution.An accurate account of the Mesozoic geologic history of the Gulf of Mexico must consider the apparent consanguinity of all magmatic rocks of the region, including the Alderdice Bank basalt, and the apparent basinward decrease in age of magmatic activities.  相似文献   

A sonic well log of the basement complex of the Walvis Ridge     

Philip D. Rabinowitz  Peter E. Borella 《Geo-Marine Letters》1983,3(1):1-7

A sonic well log was obtained within the basement complex of the Walvis Ridge during Deep Sea Drilling Project Leg 74. The top of the basement complex is characterized by smooth acoustic reflectors. The rocks recovered within the basement complex consist of basalts with intercalated sediments. According to the log ～-50% of the upper 75 m of basement are igneous rocks and the other 50% sedimentary. Sonobuoy results indicate that the ratio of sediments to basalt increases with depth for an additional 225 m until a typical oceanic velocity structure is observed. Paleontological results suggest that the processes forming this upper 300 m of the basement complex was accomplished within a short time interval.  相似文献   

Unusual large-scale phytoplankton blooms in the equatorial Pacific   总被引：1，自引：0，他引：1  

John P. Ryan  Paulo S. Polito  Peter G. Strutton  Francisco P. Chavez 《Progress in Oceanography》2002,55(3-4)

Unusual large-scale accumulations of phytoplankton occurred across 10,000 km of the equatorial Pacific during the 1998 transition from El Niño to La Niña. The forcing and dynamics of these phytoplankton blooms were studied using satellite-based observations of sea surface height, temperature and chlorophyll, and mooring-based observations of winds, hydrography and ocean currents. During the bloom period, the thermocline (nutricline) was anomalously shallow across the equatorial Pacific. The relative importance of processes that enhanced nutrient flux into the euphotic zone differed between the western and eastern regions of the blooms. In the western bloom region, the important vertical processes were turbulent vertical mixing and wind-driven upwelling. In contrast, the important processes in the eastern bloom region were wave-forced shoaling of nutrient source waters directly into the euphotic zone, along-isopycnal upwelling, and wind-driven upwelling. Advection by the Equatorial Undercurrent spread the largest bloom 4500 km east of where it began, and advection by meridional currents of tropical instability waves transported the bloom hundreds of kilometers north and south of the equator. Many processes influenced the intricate development of these massive biological events. Diverse observations and novel analysis methods of this work advance the conceptual framework for understanding the complex dynamics and ecology of the equatorial Pacific.  相似文献   

Fracture activity: A possible triggering mechanism for slope instabilities in the Eastern Atlantic?     

Peter Holler 《Geo-Marine Letters》1985,5(4):211-216

The largest known submarine slope instabilities occur on gently inclined slopes or in the deep sea. The sedimentation rates are mostly too low to induce an excess pore-water pressure sufficient to create failure. A possible triggering mechanism for these instabilities is additional horizontal ground acceleration caused by earthquakes. Old zones of weakness, represented by fracture zones, can be reactivated by isostatic movements and induce seismic activity. The distribution of some major slope instabilities and the trend of fracture zones in the Eastern Atlantic are compared and Fracture activity is suggested as the main triggering mechanism for these slope instabilities.  相似文献   

The Biology of Upogebia pusilla (Petagna) (Decapoda, Thalassinidea) I. The Burrows     

Peter C.  Dworschak 《Marine Ecology》1983,4(1):19-43

Abstract. The biology of the thalassinidean shrimp Upogebia pusilla was studied on a tidal flat in the Lagoon of Grado (Northern Adriatic). Burrows were investigated using in situ resin casting and with additional in situ and laboratory observations. Burrows show a basic pattern consisting of a U or a double U with turning chambers and a vertical shaft. Mean burrow diameter depends on animal size, it is smaller than the rigid carapace of the animal. Dimensions, distance between openings, depth of U, total depth, volume and surface are size dependent. The burrow wall is smooth and oxidized. Burrows are always inhabited by a single shrimp. Although they overlap, they are never interconnected. They are mainly constructed by compression of the sediment and are relatively permanent structures. A comparison of the burrows of Thalassinidea with regard to shape, number and appearance of openings, dimensions, properties of the burrow wall and dynamics is given.  相似文献   

Pollock (Pollachius virens) stock structure in the Canadian Maritimes inferred from mark-recapture studies     

Neilson  John D.; Stobo  Wayne T.; Perley  Peter 《ICES Journal of Marine Science》2006,63(4):749-765

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