A negative search for an ultra-slow component to the source of the Yunnan earthquakes of May 29, 1976     

Emile A. Okal  Lisa M. Stewart 《Physics of the Earth and Planetary Interiors》1981,26(3):208-216

Following Nagamune's suggestion of a giant, but very slow, component to the source of the Yunnan earthquakes of May 29, 1976, a systematic study of the ultra-low frequency content of a number of tiltmeter, strainmeter, and IDA records of the events is conducted. First, Nagamune's hypothesis is quantified, and it is found that it would require a moment in the range 10²⁹–10³⁰ dyn-cm. Such a large moment would have important consequences for our understanding of stress release in the plates, but is incompatible with the extent of the aftershock zone, and with observations on other instruments: specifically, only one IDA record shows a time-domain oscillation which may be related to the proposed source. In the Fourier domain, however, a spectral analysis fails to identify any of the Earth's modes in any of the available records, including the one originally used by Nagamune. It must therefore be concluded that the apparent signal present in a few records is due to noise—probably of instrumental origin—rather than to an ultra-low-frequency component of the seismic source.  相似文献   

Effects of tidal shallowing and deepening on phytoplankton production dynamics: A modeling study     

Lisa V. Lucas  James E. Cloern 《Estuaries and Coasts》2002,25(4):497-507

Processes influencing estuarine phytoplankton growth occur over a range of time scales, but many conceptual and numerical models of estuarine phytoplankton production dynamics neglect mechanisms occurring on the shorter (e.g., intratidal) time scales. We used a numerical model to explore the influence of short time-scale variability in phytoplankton sources and sinks on long-term growth in an idealized water column that shallows and deepens with the semidiurnal tide. Model results show that tidal fluctuations in water surface elevation can determine whether long-term phytoplankton growth is positive or negative. Hourly-scale interactions influencing weekly-scale to monthly-scale phytoplankton dynamics include intensification of the depth-averaged benthic grazing effect by water column shallowing and enhancement of water column photosynthesis when solar noon coincides with low tide. Photosynthesis and benthic consumption may modulate over biweekly time scales due to spring-neap fluctuations in tidal range and the 15-d cycle of solar noon-low tide phasing. If tidal range is a large fraction of mean water depth, then tidal shallowing and deepening may significantly influence net phytoplankton growth. In such a case, models or estimates of long-term phytoplankton production dynamics that neglect water surface fluctuations may overestimate or underestimate net growth and could even predict the wrong sign associated with net growth rate.  相似文献   

Book review     

Lisa E. Wells  John S. Perry  Iddo Wernick 《Climatic change》1996,32(1):111-119

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Immunohistochemical detection of proliferating cell nuclear antigen (PCNA) in tissues of aquatic animals utilized in toxicity bioassays     

Lisa S. Ortego  William E. Hawkins  William W. Walker  Rena M. Krol  William H. Benson 《Marine environmental research》1995,39(1-4)

Cell proliferation is an important component of toxic and carcinogenic mechanisms. A recently developed immunohistochemical assay for proliferating cell nuclear antigen (PCNA) identifies an endogenous marker for cell proliferation in routinely-fixed and paraffin-embedded specimens. This assay was adapted to identify proliferating cells in tissues of several fish species used in toxicity bioassays: medaka (Oryzias latipes), guppy (Poeata), and western mosquitofish (Gambusia affinis). The present studies show that this PCNA technique can identify proliferating cells in aquatic animals if attention is given to primary fixative, primary antibody, protein blocking reagent and antigen retrieval processing. PCNA immunoreactivity was demonstrated in tissues with normally high cell turnover such as gill, gastrointestinal tract and testis. Proliferation was also demonstrated in carcinogen-induced hepatic neoplasms.  相似文献   

Annual precipitation in the Yellowstone National Park region since AD 1173   总被引：1，自引：0，他引：1  

Stephen T. Gray  Lisa J. Graumlich 《Quaternary Research》2007,68(1):18-27

Cores and cross sections from 133 limber pine (Pinus flexilis James) and Douglas fir (Pseudotsuga menziesii (Mirbel) Franco) at four sites were used to estimate annual (July to June) precipitation in the Yellowstone National Park region for the period from AD 1173 to 1998. Examination of the long-term record shows that the early 20th century was markedly wet compared to the previous 700 yr. Extreme wet and dry years within the instrumental period fall within the range of past variability, and the magnitude of the worst-case droughts of the 20th century (AD 1930s and 1950s) was likely equaled or exceeded on numerous occasions before AD 1900. Spectral analysis showed significant decadal to multidecadal precipitation variability. At times this lower frequency variability produces strong regime-like behavior in regional precipitation, with the potential for rapid, high-amplitude switching between predominately wet and predominately dry conditions. Over multiple time scales, strong Yellowstone region precipitation anomalies were almost always associated with spatially extensive events spanning various combinations of the central and southern U.S. Rockies, the northern U.S.-Southern Canadian Rockies and the Pacific Northwest.  相似文献   

THE ASIAN TSUNAMI, ACADEMICS AND ACADEMIC RESEARCH     

Sophia Buranakul  Carl Grundy-Warr  Ben Horton  Lisa Law  Jonathan Rigg  May Tan-Mullins 《Singapore journal of tropical geography》2005,26(2):244-248

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Author Index     

Andrew L. Macumber  R. Timothy Patterson  Lisa A. Neville  Hendrik Falck 《Journal of Paleolimnology》2003,29(4):511-511

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STRANGE COUNTRIES AND SECRET WORLDS IN RUTH RENDELL'S CRIME NOVELS*     

Lisa Kadonaga 《Geographical review》1998,88(3):413-428

ABSTRACT. Mystery novels and academic geography have not often intersected. Yet crime fiction can incorporate spatial relationships and real-life regional characteristics. In recent decades mysteries have been freed from the long tradition of presenting elaborate puzzles, and now they feature human interactions in realistic settings. Writers like Ruth Rendell integrate place into their character development and plot lines. Rendell depicts changing urban landscapes in late-twentieth-century England and effectively explores contemporary British culture.  相似文献   

Ar/Ar ages and paleomagnetism of São Miguel lavas, Azores     

Catherine L. Johnson  Jan R. Wijbrans  Catherine G. Constable  Jeff Gee  Hubert Staudigel  Lisa Tauxe  Victor-H. Forjaz  Mrio Salgueiro 《Earth and Planetary Science Letters》1998,160(3-4):637-649

We present new ⁴⁰Ar/³⁹Ar ages and paleomagnetic data for São Miguel island, Azores. Paleomagnetic samples were obtained for 34 flows and one dike; successful mean paleomagnetic directions were obtained for 28 of these 35 sites. ⁴⁰Ar/³⁹Ar age determinations on 12 flows from the Nordeste complex were attempted successfully: ages obtained are between 0.78 Ma and 0.88 Ma, in contrast to published K–Ar ages of 1 Ma to 4 Ma. Our radiometric ages are consistent with the reverse polarity paleomagnetic field directions, and indicate that the entire exposed part of the Nordeste complex is of a late Matuyama age. The duration of volcanism across São Miguel is significantly less than previously believed, which has important implications for regional melt generation processes, and temporal sampling of the geomagnetic field. Observed stable isotope and trace element trends across the island can be explained, at least in part, by communication between different magma source regions at depth. The ⁴⁰Ar/³⁹Ar ages indicate that our normal polarity paleomagnetic data sample at least 0.1 Myr (0–0.1 Ma) and up to 0.78 Myr (0–0.78 Ma) of paleosecular variation and our reverse polarity data sample approximately 0.1 Myr (0.78–0.88 Ma) of paleosecular variation. Our results demonstrate that precise radiometric dating of numerous flows sampled is essential to accurate inferences of long-term geomagnetic field behavior. Negative inclination anomalies are observed for both the normal and reverse polarity time-averaged field. Within the data uncertainties, normal and reverse polarity field directions are antipodal, but the reverse polarity field shows a significant deviation from a geocentric axial dipole direction.  相似文献   

U-Pb zircon geochronology of late Neoproterozoic–Early Cambrian granitoids in Iran: Implications for paleogeography, magmatism, and exhumation history of Iranian basement     

Jamshid Hassanzadeh  Daniel F. Stockli  Brian K. Horton  Gary J. Axen  Lisa D. Stockli  Marty Grove  Axel K. Schmitt  J. Douglas Walker 《Tectonophysics》2008,451(1-4):71-96

Eurasia has largely grown to its present enormous size through episodic addition of crustal blocks by recurring birth and demise of oceans such as Paleotethys and Neotethys. Excluding the Kopet Dagh Mountains in the northeast, crystalline basement rocks of various dimensions are exposed in all continental tectonic zones of Iran. These rocks have traditionally been viewed as continental fragments with Gondwanan affinity and summarily been assigned Precambrian or younger ages, despite the fact that evidence from isotopic dating has largely been lacking. This study presents new ion microprobe and thermal-ionization zircon U-Pb geochronological data from granitoids and orthogneisses from several locations in central Iran and the Sanandaj–Sirjan structural zones to determine crystallization ages and investigate the origin and continental affinity of these various crustal fragments. The resulting U-Pb crystallization ages for the granites and orthogneisses range from late Neoproterozoic to Early Cambrian, matching the mostly juvenile Arabian–Nubian shield and Peri-Gondwanan terranes constructed after the main phase of Pan-African orogenesis. TIMS analyses of zircons with inherited cores from western Iran suggest that the Neoproterozoic crust of Iran might not be entirely juvenile, pointing to the potential presence of inherited older Proterozoic components as is common in the eastern Arabian shield. More importantly, the new zircon U-Pb crystallization ages unequivocally demonstrate that crystalline basement underlying the Sanandaj–Sirjan zone, central Iran, and the Alborz Mountains is composed of continental fragments with Gondwanan affiliation, characterized by wide spread late Neoproterozoic subduction-related magmatism. The exposure of these late Neoproterozoic–Early Cambrian basement rocks in the Iranian regions north of the Zagros is structurally controlled and linked to both large-scale crustal extension and exhumation during Mesozoic and Tertiary time as well as Tertiary collisional tectonics associated with the closure of Neotethys.  相似文献