北美斑岩矿床的某些时空概念     

Davl.  JF 杨宗镜 《西北地质》1991,(A00):33-39

  相似文献   

Facets of the geography of population in the Midwest     

Hart JF 《The Journal of geography》1986,85(5):201-211

"This paper explores four selected facets of the geography of population in the [U.S.] Midwest that are related to the movement of people: (1) the spread of occupance across the land; (2) the growth of the population of counties once they had been occupied; (3) the distribution of the foreign-born population; and (4) the distribution of retired people who have migrated after they have retired."  相似文献   

Measurement of DNA single-strand breaks in gill and hemolymph cells of mussels, Mytilus sp., collected on the French Atlantic Coast     

Akcha F  Tanguy A  Leday G  Pelluhet L  Budzinski H  Chiffoleau JF 《Marine environmental research》2004,58(2-5):753-756

DNA single-strand breaks were measured by the comet assay in both gill and hemolymph cells of mussels collected in 3 sampling areas of the French coast (Pointe du Castelli, Pen Bron and Saint-Nazaire Harbour). Whole mussel tissue samples were also collected for the chemical determination of PAH, PCB and heavy metal concentrations. In mussel, a higher level of DNA strand breaks was measured in gill than in hemolymph cells (p < 0.01). Despite a factor of contamination from 2 to 3 between sites, no difference in the extent of mussel DNA strand breaks was shown between sampling locations (p > 0.05), questioning the sensitivity of the assays used in biomonitoring studies.  相似文献   

以实况资料对比研究各种裸地蒸发公式     

Mahf.  JF 董颜 《地理译报》1993,12(1):15-21,F003

  相似文献   

太古代变质玄武岩和变质橄榄岩中递增热液碳...     

戴维.  JF 邹元坑 《江西地质科技》1991,18(3):165-175

  相似文献   

北美斑岩矿床的某些时空分布特征   总被引：1，自引：0，他引：1  

Davi.  JF 谢荣举 《地质科技情报》1991,10(1):63-68,54

斑岩矿床可能是北美研究最深入的一类矿床.但是,正如对斑岩岩浆及有关金属的来源一样,对地幔、俯冲、洋壳、大陆壳、前寒武纪克拉通的作用还存在着争论.矿床空间分布的有关方面,比如斑岩矿区相对于克拉通的位置值得注意.美国的斑岩矿床分布于克拉通上,而加拿大的则远离克拉通位于增生地体内.矿床之间的时间联系同样要注意.在美国西南部,许多铜矿的平均年龄为65Ma,而钼矿为25Ma;在蒙大拿州和爱达荷州中部,钼矿床平均年龄为55Ma,而蒙大拿Butte铜矿为75Ma.加拿大斑岩矿化的主要成矿期为:Cu200~175Ma和90~20Ma;Mo60~50Ma.不列颠哥伦比亚省中部的两个钼矿形成于140Ma和102Ma.总之,加拿大的Cu、Mo矿平均年龄明显早于在  相似文献   

Delineating depth to bedrock beneath shallow unconfined aquifers: a gravity transect across the Palmer River Basin   总被引：1，自引：0，他引：1  

Bohidar RN  Sullivan JP  Hermance JF 《Ground water》2001,39(5):729-736

In view of the increasing demand on ground water supplies in the northeastern United States, it is imperative to develop appropriate methods to geophysically characterize the most widely used sources of ground water in the region: shallow unconfined aquifers consisting of well-sorted, stratified glacial deposits laid down in bedrock valleys and channels. The gravity method, despite its proven value in delineating buried bedrock valleys elsewhere, is seldom used by geophysical contractors in this region. To demonstrate the method's effectiveness for evaluating such aquifers, a pilot study was undertaken in the Palmer River Basin in southeastern Massachusetts. Because bedrock is so shallow beneath this aquifer (maximum depth is 30 m), the depth-integrated mass deficiency of the overlying unconsolidated material was small, so that the observed gravity anomaly was on the order of 1 milligal (mGal) or less. Thus data uncertainties were significant. Moreover, unlike previous gravity studies elsewhere, we had no a priori information on the density of the sediment. Under such circumstances, it is essential to include model constraints and weighted least-squares in the inversion procedure. Among the model constraints were water table configuration, bedrock outcrops, and depth to bedrock from five water wells. Our procedure allowed us to delineate depth to bedrock along a 3.5 km profile with a confidence interval of 1.8 m at a nominal depth of 17 m. Moreover, we obtained a porosity estimate in the range of 39% to 44%. Thus the gravity method, with appropriate refinements, is an effective tool for the reconnaissance of shallow unconfined aquifers.  相似文献   

美国阿巴拉契亚寒武—奥陶纪被动边缘演化的控制因素     

Read  JF 曾允孚 《国外地质(成都)》1992,(2):11-26,33

  相似文献   

A spreadsheet method of estimating best-fit hydraulic gradients using head data from multiple wells   总被引：4，自引：0，他引：4  

Devlin JF 《Ground water》2003,41(3):316-320

Hydraulic gradients from planar water tables, or piezometric surfaces, and horizontal flow regimes can be quickly and conveniently calculated from data sets involving numerous wells. The matrix-solving functions of a modem spreadsheet program (Excel) were used to determine the equation of a water-table plane, Ax + By + Cz - D = 0, and the equation coefficients were then used to determine the magnitude of the hydraulic gradient, according to gradient = square root of A2 + B2/C2, and its direction, according to alpha = arctan B/A, where alpha is the angle measured from the x-axis. A pre-prepared Excel file constructed to handle data from up to 20 wells at once is available for free downloading at www.geo.ku.edu/hydro/KUHydro.html.  相似文献   

Regional estimation of base recharge to ground water using water balance and a base-flow index   总被引：4，自引：0，他引：4  

Szilagyi J  Harvey FE  Ayers JF 《Ground water》2003,41(4):504-513

Naturally occurring long-term mean annual base recharge to ground water in Nebraska was estimated with the help of a water-balance approach and an objective automated technique for base-flow separation involving minimal parameter-optimization requirements. Base recharge is equal to total recharge minus the amount of evapotranspiration coming directly from ground water. The estimation of evapotranspiration in the water-balance equation avoids the need to specify a contributing drainage area for ground water, which in certain cases may be considerably different from the drainage area for surface runoff. Evapotranspiration was calculated by the WREVAP model at the Solar and Meteorological Surface Observation Network (SAMSON) sites. Long-term mean annual base recharge was derived by determining the product of estimated long-term mean annual runoff (the difference between precipitation and evapotranspiration) and the base-flow index (BFI). The BFI was calculated from discharge data obtained from the U.S. Geological Survey's gauging stations in Nebraska. Mapping was achieved by using geographic information systems (GIS) and geostatistics. This approach is best suited for regional-scale applications. It does not require complex hydrogeologic modeling nor detailed knowledge of soil characteristics, vegetation cover, or land-use practices. Long-term mean annual base recharge rates in excess of 110 mm/year resulted in the extreme eastern part of Nebraska. The western portion of the state expressed rates of only 15 to 20 mm annually, while the Sandhills region of north-central Nebraska was estimated to receive twice as much base recharge (40 to 50 mm/year) as areas south of it.  相似文献