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		题名	作者	年代	出处	被引量
	1	Equine vi- ral arteritis 显示文摘	Stephanie A B Bell D V M Udeni B R	2006	Clin Teeh Equine Practice2006，，3：	1
	2	宁夏沙坡头地区中国新记录地衣(英文)显示文摘报道了宁夏沙坡头沙漠地区地衣3个中国新记录种:Fulgensia desertorum,Rinodina bischoffii和Seirophora orientalis,描述了3种地衣的表型特征,生态学特征及分布情况。	JOSHI Santosh JAYALAL Udeni OH Soon-Ok LI Xin-Rong JIA Rong-Liang HUR Jae-Seoun	2014	菌物学报2014，33，1：	1
	3	Detection of equine arteritis virus by real-time TaqMan reverse transcription-PCR as- say显示文摘	Udeni B R B Christian M L Topol J B	2002	Journal of Virological Methods2002，101，12：	1
	4	Phylogenetic analy-sis of S10 gene of field and laboratory strain of bluetongue virus from the Unite State显示文摘	Udeni B R Balasuriya N	1998	Virus Res1998，55，1：	1
	5	Immunogenicity and clinical protection against equine influenza by DNA vaccination of ponies显示文摘	Alida Ault Alyse M. Zajac Wing-Pui Kong J. Patrick Gorres Michael Royals Chih-Jen Wei Saran Bao Zhi-yong Yang Stephanie E. Reedy Tracy L. Sturgill Allen E. Page Jennifer Donofrio-Newman Amanda A. Adams Udeni B.R. Balasuriya David W. Horohov Thomas M. Cham	2012	Vaccine2012，，26：	1
	6	Evolving provenance in the Proterozoic Pranhita-Godavari Basin,India显示文摘The Pranhita-Godavari Basin in central eastern India is one of the Proterozoic 'Purana' basins of cratonic India.New geochronology demonstrates that it has a vast depositional history of repeated basin reactivation from the Palaeoproterozoic to the Mesozoic.U-Pb laser ablation inductively coupled plasma mass spectrometry dating of detrital zircons from two samples of the Somanpalli Group—a member of the oldest sedimentary cycle in the valley-constrains its depositional age to ~1620 Ma and demonstrates a tripartite age provenance with peaks at ~3500 Ma,~2480 Ma and ~1620 Ma,with minor age peaks in the Eoarchaean(~3.8 Ga) and at ~2750 Ma.These ages are consistent with palaeocurrent data suggesting a southerly source from the Krishna Province and Enderby Land in East Antarctica.The similarity in the maximum depositional age with previously published authigenic glauconite ages suggest that the origin of the Pranhita-Godvari Graben originated as a rift that formed at a high angle to the coeval evolving late Meosproterozoic Krishna Province as Enderby Land collided with the Dharwar craton of India.In contrast,detrital zircons from the Cycle III Sullavai Group red sandstones yielded a maximum depositional age of 970±20 Ma and had age peaks of ~2550 Ma,~1600 Ma and then a number of Mesoproterozoic detrital zircons terminating in three analyses at ~970 Ma.The provenance of these is again consistent with a southerly source from the Eastern Ghats Orogen and Antarctica.Later cycles of deposition include the overlying Albaka/Usur Formations and finally the late Palaeozoic to Mesozoic Gondwana Supergroup.	Udeni Amarasinghe Asru Chaudhuri Alan S.Collins Gautam Deb Sarbani Patranabis-Deb	2015	Geoscience Frontiers2015，6，3：	0

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