Fluid venting along Japanese trenches: tectonic context and thermal modeling     

P. Henry  S. J. Lallemant  X. Le Pichon  S. E. Lallemand 《Tectonophysics》1989,160(1-4):277-291

Large benthic chemosynthetic communities have been observed at four main locations during the Kaiko submersible dives in the Japanese trenches. They appear to be associated with venting along fractures. The first site for our observation was along the Japan and Kuril trenches where the continental margin is eroded by the subducting plate and collapses into the trench. The benthic communities there seem to be related to tension gashes parallel to the subduction vector. The other communities were found on the toe of the Nankai accretionary prism, along the frontal thrust and tension gashes. The temperature anomaly associated with one of the communities is modeled to constrain the upward flow of interstitial water. As the anomaly has a small spatial extent and as the peak thermal gradient is high, the best fitting model is to be found in a vertical upward flow at a velocity of 100 m/yr in a cylindrical conduit leading out of an underlying shallow thrust.  相似文献   

Comparative study of the behaviour of poliovirus in sterile seawater using RT-PCR and cell culture     

F. Le Guyader  M. L. Dincher  D. Menard  L. Schwartzbrod  M. Pommepuy 《Marine pollution bulletin》1994,28(12):723-726

Survival of poliovirus 1 was determined in sterile seawater at different salinity levels by detection of viral RNA by RT-PCR and comparison with tissue culture infectivity assay. Salinity appeared to have little influence on the behaviour of infectious particles: times necessary to obtain negative results by cell culture were not statistically different for the three salinities tested. Viral RNA was always detected by RT-PCR showing that in sterile medium viral particles can persist in a noninfectious form.  相似文献   

Kinetic investigation of the OH + CH3Br reaction between 248 and 390 K     

A. Chichinin  S. Teton  G. Le Bras  G. Poulet 《Journal of Atmospheric Chemistry》1994,18(3):239-245

The rate parameters for the reaction of the OH radical with CH₃Br have been measured using the discharge flow-electron paramagnetic resonance method. The result isk ₁=(1.86±0.48)×10^–12 exp[–(1230±150)/T] cm³ molecule^–1 s^–1. This value is compared to earlier data and is found to be in excellent agreement with the most recent results, which greatly increases the accuracy of the ozone depletion potential of CH₃Br which can be derived from these kinetic data.  相似文献   

Reviews     

Johanna Rosier  Richard Le Heron 《New Zealand geographer》1995,51(2):61-62

Book reviewed in this article:
Green Politics By S. Rainbow.
Keeping New Zealand Green: Recent Environmental Reforms By P.A. Memon.
Environmental Planning in New Zealand Edited by P.A. Memon and H. C. Perkins.  相似文献   

Magnetic anomalies in the Shikoku Basin: a new interpretation   总被引：1，自引：0，他引：1  

Nicolas Chamot-Rooke  Vincent Renard  Xavier Le Pichon 《Earth and Planetary Science Letters》1987,83(1-4)

Kaiko surveys over the Nankai Trough made available new magnetic and structural data for the northern Shikoku Basin. A survey of the oceanic lithosphere subducting below Southwest Japan along the central Nankai Trough revealed the existence of several north-south basement troughs. They are probably transform faults related to a north-south spreading system. We examine the possibility of a late phase of north-south spreading limited to the axial northernmost Shikoku Basin, active between 14 and 12 Ma. If this system was already active before that time, i.e. during the N55° opening of the southeastern basin, then a triple junction should be found between both areas.Based on these data and previous studies we present a new interpretation of magnetic anomalies over the whole basin. From early east-west rifting to late north-south spreading, opening of the Shikoku Basin proceeded through multiple episodes of spreading. The analysis of magnetic anomalies constrains the kinematic evolution of the basin through time and space. Two successive counter-clockwise rotations of the spreading direction are postulated, at anomaly 6 (19 Ma) and at anomaly 5B (14 Ma), involving segmentation and rotation of the spreading ridge.  相似文献   

Review of measurements of the RF spectrum of radiation from lightning   总被引：2，自引：0，他引：2  

Dr D. M. Le Vine 《Meteorology and Atmospheric Physics》1987,37(3):195-204

Summary A review is presented of the measurements reported in the literature of the spectrum of electromagnetic radiation from lightning in the frequency range from 1 kHz to 1 GHz. Measurements have been made either by monitoring the power received at inidividual frequencies using a narrow bandwidth recording device or by recording the transient (time dependent) radiation with a wide bandwidth device and then Fourier transforming the waveform to obtain a spectrum. Measurements of the first type were made extensively in the 1950's and 1960's and several composite spectra have been deduced by normalizing the data of different investigators to common units of bandwidth and distance. The composite spectra tend to peak near 5 kHz and then decrease roughly as 1/(frequency) up to nearly 100 MHz where scatter in the data make the behaviour uncertain. The spectrum obtained with measurements of the second type is similar. Recent experiments have extended the frequency range covered to several 10's of MHz and include spectra for return strokes, the stepped leader and for some intracloud processes. The spectrum of first return strokes obtained in this manner is very similar to the spectrum of the composite flash obtained from the narrowband measurements.With 9 Figures  相似文献   

Surface heat fluxes from a numerical weather prediction system     

J Y Simonot  H Le Treut 《Climate Dynamics》1987,2(1):11-28

Twenty-two months (July 1983-April 1985) of surface heat fluxes predicted at day 1 from a numerical weather prediction system have been processed. Monthly means and monthly standard deviations of available surface short-wave, long-wave, latent and sensible heat fluxes as well as annual means have been computed. The global mean of the annual net sea-surface heat flux is about 40 Wm^–2 and is therefore far from equilibrium. When used to force an oceanic model, these fluxes would tend to warm the ocean and would produce an unrealistic transport of heat by the oceanic general circulation. They therefore need to be corrected. This correction appears feasible because the main difference between these fluxes and long-term climatologies appears largely independent of the month and the latitude. This suggests that the errors have a systematic origin. The corrected fluxes allow both the reproduction of a realistic seasonal migration of the zero net heat-flux line and the reproduction of the annual meridional heat transport in the different oceans, within the range of previous estimates.  相似文献   

Wind-driven ocean circulation transition to barotropic instability     

Christian Le Provost  Jacques Verron 《Dynamics of Atmospheres and Oceans》1987,11(2)

This article deals with the ocean circulation driven by steady zonal winds, and damped by bottom and biharmonic friction, when represented by the simple barotropic vorticity equation. A double gyre antisymmetrical wind stress pattern in a square basin is considered. Wind forcing and dissipation parameters are chosen within the ranges of what has been used in previous studies. The flow characteristics for both steady and unsteady situations are tentatively described as functions of model external parameters through the analysis of a large set of numerical experiments. Functional relations are derived for the mid-latitude jet parameters (length, width and transport) on the basis of scaling arguments. With the diagrams established for these quantities in forcing and dissipation parameter relations allow quantitative predictions of model response to a wide range of parameter choices to be made. The transition to barotropic instability is interpreted by analysing and comparing the spin-up phase of different numerical experiments leading either to stable or unstable solutions. Two major types of destabilization are identified, namely through meandering of the mid-latitude eastward jet and Rossby wave radiation from the westward return flow. The characteristics of the flows are shown to be highly sensitive to the external parameter changes. Competition between eddy kinetic energy level and eastward jet extension appears to consttitute the key point of this class of solutions, controlling in particular the intensity of transport in the inner gyres, driven by the eddy field on the two sides of the mid-basin jet, in a very similar manner to that of the more complex multilayered EGCMs.  相似文献   

Kinematic evolution of the Tethys belt from the Atlantic ocean to the pamirs since the Triassic     

Lonid A. Savostin  Jean-Claude Sibuet  Lev P. Zonenshain  Xavier Le Pichon  Marie-Jos Roulet 《Tectonophysics》1986,123(1-4)

We present an updated series of kinematic reconstructions of the major plates around the Tethys from the Atlantic Ocean to the Pamirs between the Early Jurassic and the Present. This set is used elsewhere as a basis for paleogeographic maps of the entire region. The problems related to the positions of the continents in the Lower Triassic are also discussed. No direct analyses of magnetic anomalies and fracture zones in the Atlantic have been made. Rather, all available poles and rotations have been tested in order to eliminate or minimize possible kinematic errors. The reconstructions are shown for nine key geological periods which correspond to well recognized magnetic anomalies, except for the Jurassic-Cretaceous boundary and the Cretaceous-Tertiary boundary which correspond to interpolated positions. Paleolatitudes have been drawn using the study of Westphal et al. (1986). An attempt has been made to take into account the displacements caused by formation of the continental margins and basins by stretching. The resulting relative vector of motions along the northern boundary of the Tethys shows a significant change 80 m.y. ago. Left-lateral motion with compression dominates before whereas right-lateral motion with compression dominates after. To the east, rates of motion vary by a factor of three with time and four maxima can be clearly related to tectonic events in the Late Jurassic, Late Cretaceous, Eocene and post Middle Miocene. To the west, north of Apulia, on the contrary, the motion rate has not changed significantly since the Early Cretaceous and is close to 1 cm/yr as an average. These rather complex adjustments in rates and directions of relative motion are produced in great part through a complex migration of the Africa-Eurasia pole of rotation and seem to be mostly governed by the tectonics of the Tethys plate boundary.  相似文献   

Geological evolution of the tethys belt from the atlantic to the pamirs since the LIAS   总被引：3，自引：0，他引：3  

J. Dercourt  L.P. Zonenshain  L.-E. Ricou  V.G. Kazmin  X. Le Pichon  A.L. Knipper  C. Grandjacquet  I.M. Sbortshikov  J. Geyssant  C. Lepvrier  D.H. Pechersky  J. Boulin  J.-C. Sibuet  L.A. Savostin  O. Sorokhtin  M. Westphal  M.L. Bazhenov  J.P. Lauer  B. Biju-Duval 《Tectonophysics》1986,123(1-4)

We discuss nine palinspastic geological maps (Plates 1–9), at scale, which depict the evolution of the Tethys belt from the Pliensbachian (190 Ma) to the Tortonian (10 Ma). A Present structural map (Plate 10) is shown for comparison at the same scale with the same conventions. Our reconstructions are based on a kinematic synthesis (Savostin et al., 1986), a paleomagnetic synthesis (Westphal et al., 1986) and geological compilations and analyses concerning in particular the western domain (Ricou et al., 1986), the eastern passive margins (Kazmin et al., 1986a), the eastern active margins (Kazmin et al., 1986b), the Black Sea-Caspian Sea basins (Zonenshain and Le Pichon, 1986) and the ophiolites (Knipper et al., 1986).  相似文献