U–Pb Ages for Zircon Grains from Nsanaragati Alluvial Gem Placers: Its Correlation to the Source Rocks          下载免费PDF全文

Nguo Sylvestre Kanouo  Rose Fouateu Yongue  Emile Ekomane  Emmanuel Njonfang  Changqian Ma  David R. Lentz  Zhenbing She  Khin Zaw  Akella Satya Venkatesh 《Resource Geology》2015,65(2):103-121

The Mamfe Basin is located in the SW of Cameroon and is an extension of the much bigger Benue Trough in the SE of Nigeria. Along the Asenem River and its tributaries in the western part of the Mamfe Basin (close to the border with Nigeria) gem placers yielding big zircon grains were found in recent river sediments close to Nsanaragati. In order to determine the source area and to establish a possible correlation between the zircons found in the Nsanaragati placers and rocks surrounding the Mamfe Basin 56 detrital zircon grains were analysed regarding their U–Pb ages and selected trace element contents by LA‐ICP–MS techniques. Possible source areas are rocks from the Benue Trough in the West and from the Cameroon Volcanic Line (CVL) in the SE of the study area. Based on microscopic analyses it was possible to distinguish two groups of zircons: reddish and non‐reddish ones, where the latter group comprises color variations from brown to orange, yellow to even colorless. In general, the detrital zircons show high hafnium values (4576 to 12565 ppm) and very variable thorium (7.8 to 1565 ppm) and uranium values (13.4 to 687 ppm). The Th/U ratios vary from 0.4 to 2.3, allowing correlations for some zircon grains to kimberlitic, granitic or syenitic affinities. It was also possible to distinguish zircon grains crystallised in mafic mantle‐derived melts from those crystallised in felsic melts, e.g. from continental rift‐related magmatic systems. In general, the U–Pb zircon ages obtained range from 11.7 to 1949 Ma. All zircons of the reddish group yielded almost similar ages resulting in a Concordia age of 12.4 Ma (Serravallian), an age unknown from the Mamfe Basin so far. The group of non‐reddish zircons showed various ages ranging from Serravallian to Orosirian. It was possible to correlate the youngest ages with rocks known from intrusions along the CVL, dated with K/Ar or Ar/Ar methods. The most probable sources were Mount Bamenda and Mount Bambouto in the east of the Mamfe Basin. Cretaceous ages are interpreted as re‐recycled clastic sediments whose original source had been rocks in the south and the north of the Benue Trough and who had been eroded and deposited within the catchment area of the Asenem river system in the Mamfe Basin in post‐Cretaceous times. The oldest ages are assumed to represent the pan‐African and pre‐pan‐African basement of the Mamfe basin.  相似文献   

Impacts of rising air temperatures and emissions mitigation on electricity demand and supply in the United States: a multi-model comparison   总被引：2，自引：2，他引：0  

James McFarland  Yuyu Zhou  Leon Clarke  Patrick Sullivan  Jesse Colman  Wendy S. Jaglom  Michelle Colley  Pralit Patel  Jiyon Eom  Son H. Kim  G. Page Kyle  Peter Schultz  Boddu Venkatesh  Juanita Haydel  Charlotte Mack  Jared Creason 《Climatic change》2015,132(1):111-125

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Genetic programming approach for flood routing in natural channels     

C. Sivapragasam  R. Maheswaran  Veena Venkatesh 《水文研究》2008,22(5):623-628

In recognition of the non‐linear relationship between storage and discharge existing in most river systems, non‐linear forms of the Muskingum model have been proposed, together with methods to calibrate the model parameters. However, most studies have focused only on routing a typical hypothetical flood hydrograph characterized by a single peak. In this study, we demonstrate that the storage–discharge relationship adopted for the non‐linear Muskingum model is not adequate for routing flood hydrographs in natural channels, which are often characterized by multiple peaks. As an alternative, an evolutionary algorithm‐based modelling approach, i.e. genetic programming (GP), is proposed, which is found to route complex flood hydrographs accurately. The proposed method is applied for constructing a routing model for a channel reach along the Walla Walla River, USA. The GP model performs extremely well with a root‐mean‐square error (RMSE) of 0·73 m³ s^?1 as against an RMSE of 3·26 m³ s^?1 for routing the multi‐peaked hydrograph. The advantage of GP lies in the fact that, unlike other models, it establishes the routing relationship in an easy and simple mathematical form. Copyright © 2007 John Wiley & Sons, Ltd.  相似文献   

Site suitability analysis for soil and water conservation structures     

DILIP?G.?DurbudeEmail author  B.?Venkatesh 《Journal of the Indian Society of Remote Sensing》2004,32(4):399-405

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An Automated GIS Procedure for Delineating River and Lake Boundaries     

Venkatesh M Merwade 《Transactions in GIS》2007,11(2):213-231

Digitization of river and lake boundaries is an essential task in several hydrologic studies, which, in most cases, is performed manually by using aerial photographs. This paper presents an automatic geographic information system (GIS) procedure for delineating river and lake boundaries using aerial photographs. The GIS procedure is based on supervised classification of aerial photographs by using the National Hydrography Dataset (NHD) for creating training areas. Four study areas – Lake Palestine in Texas, Brazos River in Texas, Neuse River in North Carolina, and Snake River in Idaho – are used to demonstrate the approach. The results from the automatic boundary delineation process are evaluated by comparing them to manually digitized boundaries. The boundaries delineated by the automatic procedure matched the manually digitized boundaries with an overall difference of less than five percent in terms of area measurement. Besides saving about 85 percent of manual labor, the GIS procedure provides a consistent way of delineating water bodies, and provides estimation of river channel widths, which, in conjunction with existing NHD data, can be used to estimate average flow depths. Supplementing the regional scale NHD data with local scale attributes such as channel width and depth may lead to increased use of NHD in local scale studies.  相似文献   

Value addition of paper coating grade kaolins by the removal of ultrafine coloring impurities     

P. Raghavan  Sathy Chandrasekhar  A.D. Damodaran 《International Journal of Mineral Processing》1997,50(4):307-316

Two kaolin samples from the southern part of Kerala (A and B) have been characterised. The colouring impurities present were found to be carbonaceous and ferruginous, being also present in ultrafine size ranges. Modern beneficiation techniques such as ultra flotation and high gradient magnetic separation (HGMS) have been carried out to reduce the level of these contaminants and to increase the brightness of the product clays. The results showed that nearly 70% of the ultrafine carbonaceous matter in A, which originally contains 0.13% carbon (as fixed carbon), could be removed by shear floc-flotation. HGMS treatment could remove ∼ 45% of the iron minerals (feed assay 0.58% Fe₂O₃). Sample B contained 0.32% Fe₂O₃ and 0.19% carbon. The shear floc-flotation was found to be the only effective method by which ∼ 75% of the carbon could be floated out. This sample did not respond to HGMS which may be because of the ‘structural’ nature of the iron present. Both the kaolins, after processing, were found suitable for paper coating. Another important aspect of this work is the establishment of maximum permissible level for carbon in paper coating grade clays since the standard specifications do not give any limiting value.  相似文献   

Assessment of CMIP5 historical simulations of rainfall over Southeast Asia     

Raghavan  Srivatsan V  Liu  Jiandong  Nguyen  Ngoc Son  Vu  Minh Tue  Liong  Shie-Yui 《Theoretical and Applied Climatology》2018,132(3-4):989-1002

Theoretical and Applied Climatology - We present preliminary analyses of the historical (1986–2005) climate simulations of a ten-member subset of the Coupled Model Inter-comparison Project...  相似文献   

Regional climate simulations over Vietnam using the WRF model     

S. V. Raghavan  M. T. Vu  S. Y. Liong 《Theoretical and Applied Climatology》2016,123(1-2):161-170

Time-irreversible symmetry is a fundamental property of nonlinear time series. Time-irreversible behaviors of mean temperature measured on 182 stations over China from 1960 to 2012 are analyzed by directed horizontal visibility graph (DHVG for short), and significance of results has been estimated by Monte Carlo simulations. It is found that dominated time irreversibility emerges in nearly all daily temperature anomaly variations over China. Further studies indicate that these time-irreversible behaviors result from asymmetric distributions of persistent daily temperature increments and decrements, and this kind of symmetry can be quantified by distributions of consecutive daily mean temperature increasing or decreasing steps. At the same time, the findings above have been confirmed by artificially generated time series with given value of multiscale asymmetry.  相似文献   

Real-time application of an oil spill movement prediction system     

V. R. Neralla  S. Venkatesh 《Natural Hazards》1989,2(1):31-44

This paper deals with the prediction, in real time, of the motion of experimental oil slicks. The experiments were conducted during September 1983 offshore near Halifax on the east coast of Canada. The objectives of the experiments were (i) to determine the suitability of oil spill dispersants as countermeasures and (ii) the testing and verification of oil spill trajectory models and systems.The Atmospheric Environment Service (AES) participated in the experiments to test the capability of its oil spill motion prediction system in providing real-time trajectory forecasts. The experiment consisted of three sets of spills. Each set had a control slick and a test slick. Sixteen barrels of crude oil were used in each spill. The test slicks were used to test the effectiveness of various dispersants, the control slicks were used to verify trajectory forecasts.The spill trajectories and oil weathering information obtained from the system during the experiments demonstrated the relative ease with which the system could handle the required input and provide timely forecasts. The accuracy of these forecast trajectories was confirmed by observations, and their utility was demonstrated by their application in the operational decision-making process.  相似文献   

Tibetan anticyclone and tropical easterly jet   总被引：2，自引：0，他引：2  

K. Raghavan 《Pure and Applied Geophysics》1973,110(1):2130-2142

Summary During the summer monsoon the upper tropospheric subtropical anticyclone of Asia is centred over SE Tibet (when it is called the Tibetan anticyclone). Further, the equatorward outflow from this anticyclone gains easterly angular momentum and therefore it appears as an easterly jet stream over SE Asia south of 20N between 150 mb and 100 mb. On finding these current concepts questionable, this study offers an alternative explanation for the migration of the upper tropospheric anticyclone to the Tibetan Plateau and also for the development of the tropical easterly jet. In summer the Bay of Bengal is cold compared to its adjoining continental plains in the north. Therefore in the beginning of summer the lower levels of the anticyclone migrate from their winter position in the Bay of Bengal to the warm plains in the north. As they reach the plains by about June, the upper levels of the anticyclone above 150 mb extend north over the Tibetan Plateau irrespective of whether the Plateau is a warm source or cold source because the upper levels of the subtropical anticyclone have a characteristic poleward slope in all seasons. By about July, when the lower levels of the anticyclone migrate from the plains to still warmer areas in the north over the Plateau, the upper levels which are already over the Plateau continue to remain there throughout the season. The zonal component of the equatorward outflow from the Tibetan anticyclone computed from the law of conservation of angular momentum does not bear any comparison with the observed winds in the upper troposphere over India. On the other hand the winds computed from a thermal gradient show a reasonable agreement with the observed winds indicating thereby that the upper tropospheric high winds are thermally generated. These high winds have been found as a unique phenomenon distinct from a jet stream and therefore it is considered appropriate to call them Tropical Strong Easterlies (TSE) rather than as a tropical easterly jet stream. Some of the characteristic features of the TSE are discussed and they are ascribed to the peculiar temperature distribution in the atmosphere between 200 mb and 60 mb mainly brought about by the vertical motion associated with the summer monsoon.  相似文献