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14篇 您的检索式:作者名="MA Lichi"
    题名 作者 年代 出处 被引量
1Comparison of arterial spin labeling techniques and dynamic susceptibility weighted contrast - enhanced MRI in perfusion imaging of normal brain tissue 显示文摘Weber MA Gunther M Lichy MP 2003Invest Radiol2003,38,11:1
2Assessment of irradiated brain metastases by means of arterial spin-labeling and dynamic susceptibility-weighted contrast-enhanced perfusion MRI:initial results显示文摘Weber MA Thilmann C Lichy MP 2004Invest Radiol2004,39,:1
3Comparison of arterial spin-labeling techniques and dynamic susceptibility-weighted contrast-enhanced MRI in perfusion imaging of normal brain tissue显示文摘Weber MA Gunther M Lichy MP 2003Invest Radiol2003,38,11:1
4Comparison of arterial spin- |abeIing techniques and dynamic susceptibility-weighted contrast- enhanced MRI in perfusion imaging of normal brain tissue 显示文摘Weber MA GUnther M Lichy MP 2003Invest Radio12003,38,11:1
5Comparison of arterial spin-labeling techniques and dynamic susceptibility-weighted contrast-enhanced MRI in perfusion imaging of normal brain tissue显示文摘 Gunther M Lichy MP 2003Invest Radiol2003,38,11:1
6Comparison of Arterial Spin - Labeling Techniques and Dynamic Sus- ceptibility -Weighted Contrast- Enhanced MRI in Per- fusion hnaging of Normal Brain Tissue显示文摘Waber MA Gunther M Lichy MP 2003Invest Radi- ol2003,38,11:1
7Monitoring of irradiated brain metastases using MR perfusion imaging and ^1H MR spectroscopy显示文摘Weber MA Lichy MP Thilmann C 2003Radiologe2003,43,5:1
8Assessment of irradiated brain metastases by means of arterial spin labeling and dynamic susceptibility weighted contrast enhanced perfusion MRI:Initial results显示文摘Weber MA Thilmann C Lichy MP 2004Invest Radiol2004,39,5:1
9Comparison of arterial spin-labeling techniques and dynamic susceptibilitygweighted contrast-enhanced MRI in perfusion imaging of normal brain tissue显示文摘Weber MA GtintherM Lichy MP 2003Invest Radiol2003,38,11:1
10Comparison of arterial spin-labeling techniques and dynamic susceptibility-weighted contrast-enhanced MRI in perfusion imaging of normal brain tissue显示文摘Weber MA Gunther M Lichy MP 2003Invest Radiol2003,38,11:1
11Comparison of arterial spin-labeling techniques and dynamic susceptibility-weighted contrast-enhanced MRI in perfusion imaging of normal brain tissue显示文摘Weber MA Gunther M Lichy MP 2003Invest Radiol2003,38,:1
12Comparison of arterial spin labeling techniques and dynamic susceptibility weighted contrast-en- hanced MRI in perfusion imaging of normal brain tissue 显示文摘Weber MA Gunther M Lichy MP 2003Invest Radiol2003,38,11:1
13Exploration progress of the Paleogene in Jiyang Depression,Bohai Bay Basin显示文摘With increased exploration in the faulted basins of eastern China,petroleum exploration in this region has been challenged by unclear remaining petroleum resources distribution,complex reservoir and hydrocarbon enrichment patterns,and lacking of suitable exploration techniques.Aiming at resolving these problems,studies on source rocks,reservoirs,hydrocarbon accumulation and geophysical prospection were carried out by laboratory analysis,reservoir anatomy,and seismic analysis.A highlyefficient hydrocarbon generation/expulsion model of source rocks in saline environment was established,which aided in the discovery of a new set of source rocks in the Jiyang Depression.This study also reveals the formation process of high-quality reservoir by alternating acid and alkaline fluids during deposition and diagenesis,and pattern of secondary pores development in deep clastic rocks.Through the fine anatomy of the oil reservoirs,an orderly distribution pattern of the oil reservoirs is established,and the potential exploration targets in the undrilled area are identified.In addition,single-point highdensity seismic acquisition and high-resolution imaging technologies are developed,enabling fine and efficient exploration in areas with high exploration maturity.The research result plays a leading and demonstrative role in the fine and efficient exploration of faulted basins in eastern China.Lichi Ma Mingshui Song Yongshi Wang Yanguang Wang Huimin Liu 2023Energy Geoscience2023,4,1:0
14Shale Lithofacies and Sedimentary Environment of the Third Member,Shahejie Formation,Zhanhua Sag,Eastern China显示文摘Researches into shale lithofacies,their sedimentary environments and relationship benefit understanding both of sedimentary cycle division and unconventional hydrocarbon exploration in lacustrine basins.Based on a 100~300-m-thick dark shale,mudstone and limestone encountered in the lower third member of the Eocene Shahejie Formation(Es3l member)in Zhanhua Sag,Bohai Bay Basin,eastern China,routine core analysis,thin sectioning,scanning electron microscopy(SEM),mineralogical and geochemical measurements were used to understand detailed facies characterization and paleoclimate in the member.This Es3l shale sediment includes three sedimentary cycles(C3,C2 and C1),from bottom to top,with complex sedimentary characters and spatial distribution.In terms of the composition,texture,bedding and thickness,six lithofacies are recognized in this succession.Some geochemical parameters,such as trace elements(Sr/Ba,Na/Al,V/Ni,V/(V+Ni),U/Th),carbon and oxygen isotopes(δ^(18)O,δ^(13)C),and total organic carbon content(TOC)indicate that the shales were deposited in a deep to semi-deep lake,with the water column being salty,stratified,enclosed and reductive.During cycles C3 and C2 of the middle-lower sections,the climate was arid,and the water was salty and stratified.Laminated and laminar mudstone-limestone was deposited with moderate organic matter(average TOC 1.8%)and good reservoir quality(average porosity 6.5%),which can be regarded as favorable reservoir.During the C1 cycle,a large amount of organic matter was input from outside the basin and this led to high productivity with a more humid climate.Massive calcareous mudstone was deposited,and this is characterized by high TOC(average 3.6%)and moderate porosity(average 4%),and provides favorable source rocks.ZHU Xiaomin ZHANG Meizhou ZHU Shifa DONG Yanlei LI Chao BI Yuequan MA Lichi 2022Acta Geologica Sinica(English Edition)2022,96,3:0
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