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		题名	作者	年代	出处	被引量
	1	Why is end-of-life care delivery sporadic? : A quantitative look at the harriers to and facilitators of providing end-of-life care in the neo- natal intensive care unit显示文摘	Wright V Prasun MA Hitgenberg C	2011	Adv Neonatal Care2011，11，1：	1
	2	Mars phoenix entry, descent, and landing trajectory and atmosphere reconstruction显示文摘	Robert C B Prasun N D	2011	Journal of Spacecraft and Rockets2011，48，5：	1
	3	Why is end of life care delivery sporadic a quantitative look at the barriers to and facilitators of providing end of life care in the neonatal in- tensive care unit 显示文摘	Wright V Prasun MA Hilgenberg C	2011	Advances Neonatal Care2011，11，1：	1
	4	Evolution of landscape in a piedmont section of Eastern Himalayan foothills along India-Bhutan border: A tectono-geomorphic perspective显示文摘The present study area involves part of a deformed coalesced fan located along the Himalayan Frontal Thrust(HFT)on the east of river Tista near the India-Bhutan border.The area is marked by two spectacular E-W trending south-sloping scarps namely the Matiali(ca.60 m)and Chalsa(ca.90 m)Scarps and a north-sloping E-W trending Thaljhora(ca.80 m)Scarp.Our work comprises of a comparative study of geomorphology and geologic history in the adjacent interfluves of Jaldhaka-Gathia and Neora-Murti rivers to understand the tectonic history of the area.We mapped the Jaldhaka-Gathia river interfluve at a 1:25,000 scale and report a hitherto unidentified northerly sloping small scarp of ca.5 m height named the Nagrakata Scarp.This scarp was identified using satellite images,DEMs,and total station survey.We interpret that the two northsloping,E-W trending scarps(Thaljhora and Nagrakata Scarps)are manifestations of steep limbs of anticlines over blind south-dipping back thrusts.Together they form a wrinkle-ridge pair behind the north-dipping HFT,which is manifested by south-sloping Chalsa Scarp.We propose a plausible geomorphic model interpreting that deformation along the small fan in the Jaldhaka-Gathia interfluves is younger compared to fan deposition and deformation in the adjacent Mal-Murti interfluve.The most recent geomorphology of the Jaldhaka-Gathia interfluve is controlled by tectonism associated with the thrust below the Nagrakata Scarp where the youngest deformation episode is recorded to at around^6 ka and is likely related to motion on a splay off of the thrust beneath the Thaljhora Scarp.	Chandreyee CHAKRABARTI GOSWAMI Prasun JANA John C WEBER	2019	Journal of Mountain Science2019，16，12：	1
	5	Mars phoenix entry,descent,and landing trajectory and atmosphere reconstruction显示文摘	Robert C B Prasun N D	2011	Journal of Spacecraft and Rockets2011，48，5：	1
	6	Exploration of the inter-nal cavity of histone deacetylase(HDAC)with selec-tive HDAC1/HDAC2 inhibitors(SHI-1:2)显示文摘	JOEY L M PRASUN K C	2008	Bioorg Med Chem Lett2008，18，3：	1
	7	Why is end-of-life care delivery sporadic:a quantitative look at the barriers to and facilitators of pro- viding end-of-life care in the neonatal intensive care unit 显示文摘	Wright V Prasun MA Hilgenberg C	2011	Advances Neonatal Care2011，11，1：	1
	8	Singularity and controllability analysis of parallel manipulators and closed-loop mechanisms显示文摘	PRASUN C ASHITAVA G	2000	Mechanism and Machine Theory2000，35，：	1

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