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16篇 您的检索式：作者名="CaumonE"

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		题名	作者	年代	出处	被引量
	1	Building and editing a sealed geological model显示文摘	Guillaume Caumon Francois Lepage Charles H Sword	2004	Mathematical Geology2004，36，4：	1
	2	Towards Stochastic Time-Varying Geolog- ical Modeling 显示文摘	Guillaume Caumon	2010	Mathematical Geosciences2010，42，：	1
	3	Dynamic data integration for structural modeling : model screening approach using a distance based model parameterization显示文摘	Suzuki S Caumon G Caers J	2008	Computational Geosciences2008，12，1：	1
	4	Building andediting a sealed geological model显示文摘	CAUMON G LEPAGE F SWORD C	2004	MathematicalGeology2004，36，4：	1
	5	Stochastic Simulations of Fault Networks in 3D Structural Modeling显示文摘	Nicolas Cherpeau Guillaume Caumon Bruno Le'vy	2010	Comptes Rendus Geosciences2010，342，：	1
	6	High fH2-fS2 Conditions Associated with Sphalerite in Latala Epithermal Base and Precious Metal Deposit, Central Iran: Implications for the Composition and Genesis Conditions of Sphalerite显示文摘This paper presents the properties of fluid inclusions found in sphalerite from Latala epithermal base and precious metal deposit(Central Iran),which is hosted in Cenozoic volcanicsedimentary host-rocks.The Latala Deposit represents an example of vein type,base metal deposits in the Miduk porphyry copper deposits(PCDs)in southern Urumieh-Dokhtar magmatic belt(UDMB).Mineralization in Latala epithermal base and precious metal vein type formed in 3 stages and sphalerite-quartz veins occur in stages 2 and 3.Stage 2 quartz-sphalerite veins are associated with chalcopyrite and zoned sphalerite,along with quartz+hematite,and Stage 3 quartz-sphalerite veins contain galena+sphalerite+chalcopyrite and quartz with overgrowth of calcite.Mineralization in Stage 3 occurs as replacement bodies and contains Fe-poor sphalerite without zoning in the outer parts of the deposit.This paper focuses on fluid inclusions in veins bearing sphalerite and quartz.The fluid inclusion homogenization temperatures and salinity in sphalerite(some with typical zoning)range from 144 to 285℃and from 0.2 wt.%to 7.6 wt.%NaCl eq.Sphalerite and fluid inclusions of the Latala base and precious metal deposit formed from relatively low-T and low-salinity solutions.Raman spectroscopy analyses indicate a high percentage of CO2 in the gas phase of fluid inclusions in Fe-poor sphalerites,as expected with melting temperature for CO2 of-56.6℃,and significant amounts of H2.Lack of reduced carbon species(methane and lighter hydrocarbons)was confirmed in the petrographic study using UV light and Raman spectroscopy.High amounts of H2 in fluid inclusions of Fe-poor sphalerite can be the result of different intensities of alteration and diffusion processes.The common occurrences of CO2 in fluid inclusions have originated from magma degassing and dissolution of carbonates.Theδ^34S values for sulfide minerals in galena of sphalerite bearing veins vary between-9.8‰and-1.0‰,and theδ^34S values calculated for H2 S are between-7.1‰and+0.6‰.These values correspond to magmatic sulfur whit possible interaction with wall rocks.Magmatic fluids were successively diluted during cooling and continuous ascent.Secondary boiling would lead to variable amounts of potassic or prophylactic alteration and the hydrogen diffusion into the inclusions hosted in sphalerite of Latala.	Fariba Padyar Mohammad Rahgoshay Alexander Tarantola Marie-Camille Caumon Seyed Mohammad Pourmoafi	2020	Journal of Earth Science2020，31，3：	1
	7	Surface-Based 3D Modeling of Geological Structures显示文摘	G. Caumon P. Collon-Drouaillet C. Le Carlier de Veslud S. Viseur J. Sausse	2009	Mathematical Geosciences2009，，8：	1
	8	Nutrition and protein energy homeostasis in elderly显示文摘	Boirie Y Morio B Caumon E	2014	Mech Ageing Dev2014，1367，：	1
	9	Nutritionandproteinenergyhomeostasisinelderly显示文摘	BoirieY MorioB CaumonE etal	2014	MechAgeingDev2014，，：	1
	10	Building and Editing a Sealed Geological Model显示文摘	Guillaume Caumon Fran?ois Lepage Charles H. Sword Jean-Laurent Mallet	2004	Mathematical Geology2004，，4：	1
	11	Stochastic Simu-lations of Fault Networks in 3D Structural Modeling显示文摘	Cherpeau N Caumon G Levy B	2010	Comptes Rendus Geosciences2010，342，：	1
	12	Surface-based 3D modeling of geological structures显示文摘	Caumon G Collon-Drouaillet P Le Carlier de Veslud C	2009	MathematicalGeosciences2009，41，8：	1
	13	Reservoir flow uncertainty assessment using response surface constrained by secondary information 显示文摘	Emmanuel Fetel Guillaume Caumon	2008	Journal of Petroleum Science and Engineering2008，60，4：	1
	14	Building and Editing a Sealed Geological Model显示文摘	Guillaume Caumon Fran?ois Lepage Charles H. Sword Jean-Laurent Mallet	2004	Mathematical Geology2004，，4：	1
	15	Building and editing a sealed geological model显示文摘	CAUMON G LEPAGE F SWORD C	2004	Mathematical Geology2004，36，4：	1
	16	Concurrent number cruncher:A GPU implementation of a general sparse linear solver显示文摘	Buatois L Caumon G Levy B	2009	International Journal of Parallel Emergent and Distributed Systems2009，24，3：	1

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