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| 1 | Middle–Upper Ordovician(Darriwilian–Early Katian) Positive Carbon Isotope Excursions in the Northern Tarim Basin, Northwest China: Implications for Stratigraphic Correlation and Paleoclimate显示文摘Three positive carbon isotope excursions are reported from Middle–Upper Ordovician in Tahe oil-gas field, northern Tarim Basin. Based on conodont biostratigraphy, the Middle Darriwilian Isotope Carbon Excursion(MDICE) and the Guttenberg Carbon Isotope Excursion(GICE) are identified from Darriwilian to Early Katian by the aid of whole-rock carbon isotope data from two well cores. Positive excursion within conodont Pygodus anserinus zone is developed in Early Sandbian, and the fluctuation range is no less than MDICE. Because the range of this excursion in the generalized global carbon isotope curve is short, previous studies paid little attention to it, and named Early Sandbian Isotope Carbon Excursion(ESICE) in this paper. Furthermore, these positive excursions are not directly related to sea level fluctuations and the MDICE and GICE identified in northern Tarim can be globally correlated to that in southern China, North America, South America, and Europe. The Saergan Fm. source rocks of Middle-Upper Ordovician in Kalpin Dawangou outcrop are in accord with the geologic time of MDICE and ESICE, and GICE have strong ties to the source rock of Lianglitag Fm. in basin. Abundant organic carbon burial is an important factor in genesis of positive isotope carbon excursions. Positive oxygen isotope excursion, conodont fauna turnover, decreased conodont total diversity, and the change of sedimentary facies indicated that dramatic changes of paleoceanographic environment of Early-Middle Ordovician in Tarim Basin started from the end of Darriwillian, and an obvious icehouse climate of Late Ordovician occurred in ESICE. | Cunge Liu Guorong Li Dawei Wang Yongli Liu Mingxia Luo Xiaoming Shao | 2016 | Journal of Earth Science2016，27，2： | 9 |
| 2 | Early dolomitisation of the Lower-Middle Ordovician cyclic carbonates in northern Tarim Basin, NW China显示文摘High-frequency metre-scale cycles are present within the Lower-Middle Ordovician carbonate successions in northern Tarim Basin, NW China. These metre-scale cycles were variably dolomitised from top to bottom. Three types of replacive dolomites were recognised, including dololaminite(very finely to finely crystalline, planar-s to nonplanar-a dolomite;type-1), patterned dolomite(finely crystalline, planar-s dolomite; type-2), and mottled dolomite(finely to medium crystalline,nonplanar-a(s) dolomite; type-3). Petrographic evidence indicate these dolomites were primarily deposited in supratidal to restricted subtidal environments, and formed in near-surface to shallow burial realms. Geochemically, all types of dolomites have similar δ13C and 87Sr/86 Sr ratios comparable to calcite precipitated in equilibrium with the Early-Middle Ordovician seawater. These geochemical attributes indicate that these dolomites were genetically associated and likely formed from connate seawater-derived brines. Of these, type-1 dolomite has δ18O values(.4.97‰ to.4.04‰ VPDB) slightly higher than those of normal seawater dolomite of the Early-Middle Ordovician age. Considering the absence of associated evaporites within type-1 dolomite, its parental fluids were likely represented by slightly evaporated(i.e., mesosaline to penesaline) seawater with salinity below that of gypsum precipitation. More depleted δ18O values(.7.74‰ to.5.20‰ VPDB) of type-2 dolomite and its stratigraphic position below type-1 dolomite indicate the generation of this dolomite from mesosaline to penesaline brines at higher temperatures in near-surface to shallow burial domains. Type-3 dolomite yields the most depleted δ18O values(–9.30‰to –7.28‰ VPDB), pointing to that it was most likely formed from coeval seawater-derived brines at highest temperatures in a shallow burial setting. There is a downward decreasing trend in δ18O values from type-1 through type-2 to type-3 dolomites, and in abundance of dolomites, indicating that the dolomitising fluids probably migrated downward from above and persisted into shallow burial conditions. | GUO Chuan CHEN DaiZhao DONG ShaoFeng QIAN YiXiong LIU CunGe | 2017 | Science China Earth Sciences2017，60，7： | 3 |
| 3 | Effect of Cyclosporine on Left Ventricular Remodeling After Reperfused Myocardial Infarction显示文摘 | Nathan Mewton Pierre Croisille Gerald Gahide Gilles Rioufol Eric Bonnefoy Ingrid Sanchez Thien Tri Cung Catherine Sportouch Denis Angoulvant Gérard Finet Xavier André-Fou?t Geneviève Derumeaux Christophe Piot Hélène Vernhet Didier Revel Michel Ovize | 2010 | Journal of the American College of Cardiology2010，，12： | 2 |
| 4 | 将老年患者的药物不良反应降到最低显示文摘老年患者承受着不可预见的药物副作用。失落、抑郁、精神错乱以及皮疹都会导致药物不良反应的发生。大约1/3使用5种以上药物的老年患者每年都会发生药物间的不良反应,这些患者中,约2/3需要医疗关注。而实际上,这些反应中,约95%可以被预料到,28%可以被预防。 | Cung B.Pham Robert L.Dickman 周泓旭 | 2008 | 中国实用乡村医生杂志2008，15，10： | 2 |
| 5 | An introduction to the European Hydrological System-Systeme Hydrologique Europeen, 'SHE', 2 :Structure of a physically-based, distributed modelling systerr显示文摘 | Abbott M B Bathurst J C Cunge J A | 1986 | Journal of Hydrology1986，87，12： | 1 |
| 6 | An introduction to the European Hydrologic System-System Hydrologique European,SHE显示文摘 | Abbott M B Bathurst J C Cunge J A | 1986 | J of Hydrol1986，87，： | 1 |
| 7 | An Introduction to the European Hydrological System-Systemc Hydrologique European,' SHE',1:History and Philosophy of a Physically-Based,Distributed Modelling System显示文摘 | Bathurst J C Cunge J A | 1986 | Journal of Hydrology1986，87，： | 1 |
| 8 | An introduction to the European Hydrological System, SHE, 1: History and Philosophy of a Physically-based Distributed Modeling System 显示文摘 | ABBOTF M B BATHURST J C CUNGE J A | 1986 | Journal of Hydrology1986，87，： | 1 |
| 9 | On then subject of flood propagation computation method (Muskingum method)显示文摘 | Cunge J A | 1969 | Hydraul Res1969，7，2： | 1 |
| 10 | Chromosomal translocations involving the IGH@ locus in B-cell precursor acute lyrnphoblastic leukemia: 29 new eases and a review of the literature显示文摘 | Chapiro E Radford-Weiss I Cung HA | 2013 | Cancer Genet2013，206，5： | 1 |
| 11 | An Introduction to the European Hydrological System-Systeme Hydrologique Europeen,' SHE ',2:Structure of a Physically Based,Distributed Modelling System显示文摘 | Bathurst J C Cunge J A | 1986 | Journal of Hydrology1986，87，： | 1 |
| 12 | An introduction to the european hydrological system-systeme hydrologique europeen, ' SHE', 2: structure of a physically-based, distributed modelling system 显示文摘 | Abbott M B Bathurst J C Cunge J A | 1986 | Journal of Hydrology1986，87，12： | 1 |
| 13 | Cleaning aluminum fluoride coatings from plasma reactor walls in SiCl4/Cl2 plasmas 显示文摘 | Ramos R Cunge G Pelissier B | 2007 | Plasma Sources Sci Technol2007，16，： | 1 |
| 14 | Design of notched gate processes in high density plasmas 显示文摘 | J Foucher G Cunge L Vallier | 2002 | J Vac Sci Technol2002，20，5： | 1 |
| 15 | On the subject of a flood propagation method (Musk ingum Method)显示文摘 | Cunge K A | 1969 | J Hydraulic R-esearch1969，7，2： | 1 |
| 16 | Synthesis of a novel fluorescent poly(D,L-lactide) end-capped with 1-pyrenebutanol used for the preparation of nanoparticles显示文摘 | Cung A N Eric A Gregoire S | 2003 | European Journal of Pharmaceutical Sciences2003，20，2： | 1 |
| 17 | An introduction to the European Hydrological System,'SHE',1:History and philosophy of a physically-based,distributed modeling system显示文摘 | Abbott M B Bathurst J C Cunge J A O'Connell P E Rasmussen J | 1986 | Journal of Hydrology1986，87，： | 1 |
| 18 | On the subject of flood propagation computa- tionmethod(Muskingum method)显示文摘 | Cunge J A | 1969 | Journal of Hy- draulic Engineering1969，7，： | 1 |
| 19 | Spray-combustion interaction mechanism of multiple- injection under diesel engine conditions 显示文摘 | Cung Khanh Moiz Abdul Johnson Jaclyn | 2015 | Proceedings of the Combustion Institute2015，35，3： | 1 |
| 20 | On the subject of flood propagation computation method (Muskingtun method)显示文摘 | CUNGE J A | 1969 | J of Hydraul Res1969，7，2： | 1 |
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