Assessment of Geochemical Anomaly Uncertainty Through Geostatistical Simulation and Singularity Analysis   总被引：1，自引：0，他引：1  

Liu  Yue  Cheng  Qiuming  Carranza  Emmanuel John M.  Zhou  Kefa 《Natural Resources Research》2019,28(1):199-212

Natural Resources Research - Geochemical anomalies are commonly separated into different geochemical anomaly levels based on one or more thresholds. However, this practice may cause some important...  相似文献   

New Discovery of Selenides in the Shiti Barite Deposit,Dabashan Region and its Geological Significances     

LIU Jiajun  DAI Hongzhang  ZHAI Degao  Emmanuel J. M. CARRANZA  YUAN Feng 《《地质学报》英文版》2020,94(2):558-560

The large-scale Shiti barite deposit of Shaanxi,being stratiform or stratoid in form,occurs in an early Paleozoic large witherite-barite metallogenic belt of southern Qinling region(China).The ore deposit,hosted in Lower Silurian Daguiping Formation,is composed of a series of carbonaceous chert,carbonaceous slate and carbonaceous sandstone,and is characterized by persistent syn-sedimentary ore beds.Barite,w itherite.barytocalcite and barite-witherite constitute the major ore minerals,with barite being the main one.  相似文献   

From 2D to 3D Modeling of Mineral Prospectivity Using Multi-source Geoscience Datasets,Wulong Gold District,China     

Zhang  Zhiqiang  Zhang  Jiaojiao  Wang  Gongwen  Carranza  Emmanuel John M.  Pang  Zong  Wang  Hao 《Natural Resources Research》2020,29(1):345-364

Natural Resources Research - The Wulong gold district (WGD) is located at the northeastern margin of the North China Carton (NCC) on the Liaodong Peninsula, China. The results of early mineral...  相似文献   

Bustylus (Eutheria, Adapisoriculidae) and the absence of ascertained marsupials in the Palaeocene of Europe     

Emmanuel Gheerbrant 《地学学报》1991,3(6):586-592

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NO<Subscript>3</Subscript> Vertical Profile Measurements from Remote Sensing Balloon-Borne Spectrometers and Comparison with Model Calculations     

Jean-Baptiste?RenardEmail author  Martyn?P.?Chipperfield  Gwena?l?Berthet  Fabienne?Goffinont-Taupin  Claude?Robert  Michel?Chartier  Howard?Roscoe  Wuhu?Feng  Emmanuel?Rivière  Michel?Pirre 《Journal of Atmospheric Chemistry》2005,51(1):65-78

Eleven vertical profiles of stratospheric NO₃ have been obtained since 1992 using the AMON and SALOMON balloon-borne UV-visible spectrometers. The measurements are compared to the SLIMCAT 3D model and calculations based on the steady-state hypothesis for NO₃. The calculations cannot reproduce some parts of the profiles which exhibit strong concentration fluctuations over few kilometres, as a consequence of the dependence of NO₃ on local temperature variations. A statistical use of the data allows us to estimate the influence of the temperature dependence of the absorption cross-section on the data analysis, and the validity of the recommended reaction rates available in the literature. Discrepancies exist between the model based on recommended kinetics and observations at warmer temperatures. Nevertheless, the analysis is biased by local temperature inhomogeneities, and only a low-resolution vertical shape of the NO₃ profiles can be retrieved.  相似文献   

Large-offset approximation to seismic reflection traveltimes   总被引：4，自引：0，他引：4  

Emmanuel Causse  Geir Ultveit Haugen  Björn Eino Rommel 《Geophysical Prospecting》2000,48(4):763-778

Conventional approximations of reflection traveltimes assume a small offset-to-depth ratio, and their accuracy decreases with increasing offset-to-depth ratio. Hence, they are not suitable for velocity analysis and stacking of long-offset reflection seismic data. Assuming that the offset is large, rather than small, we present a new traveltime approximation which is exact at infinite offset and has a decreasing accuracy with decreasing offset-to-depth ratio. This approximation has the form of a series containing powers of the offset from 1 to −∞. It is particularly accurate in the presence of a thin high-velocity layer above the reflector, i.e. in a situation where the accuracy of the Taner and Koehler series is poor. This new series can be used to gain insight into the velocity information contained in reflection traveltimes at large offsets, and possibly to improve velocity analysis and stacking of long-offset reflection seismic data.  相似文献   

Geologically Constrained Probabilistic Mapping of Gold Potential, Baguio District, Philippines   总被引：1，自引：0，他引：1  

Emmanuel John M. Carranza  Martin Hale 《Natural Resources Research》2000,9(3):237-253

Binary predictor patterns of geological features are integrated based on a probabilistic approach known as weights of evidence modeling to predict gold potential. In weights of evidence modeling, the log _e of the posterior odds of a mineral occurrence in a unit cell is obtained by adding a weight, W ⁺ or W ^– for presence of absence of a binary predictor pattern, to the log _e of the prior probability. The weights are calculated as log _e ratios of conditional probabilities. The contrast, C = W ⁺ – W ^–, provides a measure of the spatial association between the occurrences and the binary predictor patterns. Addition of weights of the input binary predictor patterns results in an integrated map of posterior probabilities representing gold potential. Combining the input binary predictor patterns assumes that they are conditionally independent from one another with respect to occurrences.  相似文献   

Using land cover changes and demographic data to improve hydrological modeling in the Sahel          下载免费PDF全文

Jean Emmanuel Paturel  Gil Mahé  Pierre Diello  Bruno Barbier  Alain Dezetter  Claudine Dieulin  Harouna Karambiri  Hamma Yacouba  Amadou Maiga 《水文研究》2017,31(4):811-824

At the beginning of the drought in the Sahel in the 1970s and 1980s, rainfall decreased markedly, but runoff coefficients and in some cases, absolute runoff increased. This situation was due to the conversion of the land cover from natural vegetation with a low annual runoff coefficient, to cropland and bare soils, whose runoff coefficients are higher. Unless they are adapted, hydrological conceptual models, such as GR2M, are unable to reproduce this increase in runoff. Despite the varying environmental and climatic conditions of the West African Sahel, we show that it is possible to increase the performance of the GR2M model simulations by elaborating a time‐varying soil water holding capacity and to incorporate this value in the annual maximum amount of water to be stored in reservoir A of the model. We looked for interactions between climate, rural society, and the environment. These interactions drive land‐cover changes in the Sahel, which in turn drive the distribution of rainfall between infiltration, evaporation, and runoff and hence the water resources, which are vital in this region. We elaborated several time series of key indicators linked to these interactions. We then integrated these changes in the runoff conditions of the GR2M model through the maximum value of the reservoir capacity. We calculated annual values of water holding capacity using the annual values of four classes of land cover, natural vegetation, cultivated area, bare soil, and surface water. We then used the hydrological model with and without this time‐varying soil value of A and compared the performances of the model under the two scenarios. Whatever the calibration period used, the Nash–Sutcliffe index was always greater in the case of the time‐varying A time series.  相似文献   

Variations of streambed vertical hydraulic conductivity before and after a flood season   总被引：1，自引：0，他引：1  

Guangdong Wu  Longcang Shu  Chengpeng Lu  Xunhong Chen  Xiao Zhang  Emmanuel K. Appiah-Adjei  Jingsi Zhu 《Hydrogeology Journal》2015,23(7):1603-1615

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‘I hate sand … it gets everywhere’—Phanerozoic sedimentary recycling from NW Africa     

James Lovell-Kennedy  Emmanuel Roquette  Stefan Schröder  Jonathan Redfern 《Basin Research》2023,35(1):187-213

Over 10,000 published detrital zircon ages have been reprocessed (applying a +10% normal and reverse concordance range) and analysed to understand the evolution of the detrital zircon record of north-west Africa during the Phanerozoic. Using dissimilarity and clustering analysis, shifts in detrital zircon populations allow interpretation of the evolution of source regions and source to sink systems throughout the Phanerozoic within the West Gondwana superfan. Previous thermochronology and field studies conducted across north-west Africa indicate significant and sustained shifts in source regions in Meso-Cenozoic times which are not recorded in the detrital zircon geochronology record. This discrepancy is most notable for Mesozoic to modern source to sink studies focused on the evolution of the Atlasic rift and opening of the Atlantic and Tethyan Oceans to the west and north respectively. Our results indicate a high degree of similarity between samples from Cambrian times onwards due to successive phases of sediment recycling. This highlights the need to integrate detrital zircon analysis with other techniques to provide confident reconstruction of sediment routing systems across Morocco. This systematic review also reveals the ubiquitous occurrence of Mesoproterozoic zircons within Moroccan sediment. No basement of this age is known from north-west Africa—often described as the ‘Mesoproterozoic Gap’, which was thought to be a diagnostic feature of sediment derived from the West African Craton. However, zircons of this age form 7% of all analysed zircons and are present in sediments from at least 700 Ma. The presence of this population is interpreted as strongly diagnostic of provenance from either the Amazonian Craton or the Eastern Gondwana Orogen within Central Africa. Their presence in the Moroccan detrital record from the Neoproterozoic onwards raises questions about the position of the West African Craton in the Proterozoic, and for the spatial extent of Mesoproterozoic orogeny within north Africa.  相似文献