目的探讨原发性中枢神经系统淋巴瘤(primary central nervous system lymphoma,PCNSL)的MRI表现,提高诊断水平。方法回顾性分析我院经病理证实的14例PCNSL患者的MRI资料。14例患者均进行MRI平扫及增强扫描,其中3例患者行MRS。由两名资深...目的探讨原发性中枢神经系统淋巴瘤(primary central nervous system lymphoma,PCNSL)的MRI表现,提高诊断水平。方法回顾性分析我院经病理证实的14例PCNSL患者的MRI资料。14例患者均进行MRI平扫及增强扫描,其中3例患者行MRS。由两名资深MRI诊断医师对MRI图像进行分析,包括病灶的部位、数目、信号特点、强化方式、瘤周水肿、囊变坏死、出血及MRS等。结果1)病灶数目14例患者中单发12例,多发2例,单发病例中有2例病变跨越两个脑叶,1例病变位于左侧小脑半球-小脑蚓部;2)病灶分布右额叶5个,左额叶5个,左顶叶2个,胼胝体2个,左侧大脑脚1个,左侧基底节2个,左右颞叶各1个,左侧小脑半球2个;3)信号特点等T110个,稍长/长T19个;等T28个,稍长/长T211个;DWI稍高信号8个,高信号11个;4)强化特点不均匀强化3例,明显均匀强化11例,软脑膜强化3例,2例多发病例中所有病灶均明显均匀强化;5)瘤周水肿重度水肿2个,中度水肿3个,轻度水肿14个;6)出血及囊变出血2个,囊变2个。结论增强、弥散加权成像联合瘤周水肿对PCNSL的诊断有重要价值,MRS对鉴别诊断有一定的作用。展开更多
目的探讨3.0 T磁共振3D-T1-可变反转角快速自旋回波(Sampling Perfection with Application Optimized Contrasts Using Different Fip Angle Evolution,3D-T1-SPACE)增强序列评估大脑中动脉(Middle Cerebral Artery,MCA)粥样硬化患者...目的探讨3.0 T磁共振3D-T1-可变反转角快速自旋回波(Sampling Perfection with Application Optimized Contrasts Using Different Fip Angle Evolution,3D-T1-SPACE)增强序列评估大脑中动脉(Middle Cerebral Artery,MCA)粥样硬化患者受累血管的临床价值。方法分析46例单侧MCA粥样硬化性狭窄患者临床、影像资料,对比评估3D-T1-SPACE增强、三维时间飞跃法磁共振血管成像(Three Dimensional Time of Flight Magnetic Resonance Angiography,3D-TOF-MRA)在测量管腔狭窄及病变长度方面与数字减影血管造影(Digtial Subtraction Angiography,DSA)的一致性。结果相比DSA,3D-T1-SPACE增强在评估管腔狭窄方面的一致性优于3D-TOF-MRA(ICC=0.91、0.80),而两者在测量病变长度方面均高于DSA(P<0.001);DSA、3D-TOF-MRA显示管腔局部轻微凹陷可疑狭窄时,3D-T1-SPACE增强序列可有效检出管壁微小斑块。结论3D-T1-SPACE增强序列能有效评估MCA粥样硬化管腔狭窄、病变长度及斑块特征,可作为MCA粥样硬化患者常规无创诊断及随访评估手段。展开更多
Precise in situ zircon U-Pb dating and Lu-Hf isotopic measurement using an LA-ICP-MS system, whole-rock major and trace element geochemistry and Sr-Nd isotope geochemistry were conducted on the volcanic host rocks of ...Precise in situ zircon U-Pb dating and Lu-Hf isotopic measurement using an LA-ICP-MS system, whole-rock major and trace element geochemistry and Sr-Nd isotope geochemistry were conducted on the volcanic host rocks of the Tongyu copper deposit on the basis of further understanding of its geological characteristics. Three zircon samples from the volcanic host rocks yielded 206Pb/238 U weighted average ages ranging from 436±4 Ma to 440±5 Ma, which are statistically indistinguishable and coeval with the ca. 440 Ma northward subduction event of the Paleo-Qinling oceanic slab. The volcanic host rocks were products of magmatic differentiation that evolved from basalt to andesite to dacite to rhyolite, forming an integrated tholeiitic island arc volcanic rock suite. The primitive mantle-normalized trace element patterns for most samples show characteristics of island arc volcanic rocks, such as relative enrichment of LILE（e.g. Th, U, Pb and La） and depletion of HFSE（e.g. Nb, Ta, Ti, Zr and Hf）. Discrimination diagrams of Ta/Yb vs Th/Yb, Ta vs Th, Yb vs Th/Ta, Ta/Hf vs Th/Hf, Hf/3 vs Th vs Nb/16, La vs La/Nb and Nb vs Nb/Th all suggest that both the volcanic host rocks from the Tongyu copper deposit and the volcanic rocks from the regional Xieyuguan Group were formed in an island arc environment related to subduction of an oceanic slab. Values of ISr（0.703457 to 0.708218） and εNd（t）（-2 to 5.8） indicate that the source materials of volcanic rocks from the Tongyu copper deposit and the Xieyuguan Group originated from the metasomatised mantle wedge with possible crustal material assimilation. Most of the volcanic rock samples show good agreement with the values of typical island arc volcanic rocks in the ISr-εNd（t） diagram. The involvement of crustal-derived material in the magma of the volcanic rocks from the Tongyu copper deposit was also reflected in the zircon εHf（t） values, which range from-3.08 to 10.7, and the existence of inherited ancient xenocrystic zircon cores（2616±39 Ma and 1297±22 Ma）. The mineralization of the Tongyu copper deposit shows syn-volcanic characteristics such as layered orebodies interbedded with the volcanic rock strata, thus, the zircon U-Pb age of the volcanic host rocks can approximately represent the mineralization age of the Tongyu copper deposit. Both the Meigou pluton and the volcanic host rocks were formed during the ca. 440 Ma northward subduction of the Paleo-Qinling Ocean when high oxygen fugacity aqueous hydrothermal fluid released by dehydration of the slab and the overlying sediments fluxed into the mantle wedge, triggered partial melting of the mantle wedge, and activated and extracted Cu and other ore-forming elements. The magma and ore-bearing fluid upwelled and erupted, and consequently formed the island arc volcanic rock suite and the Tongyu VHMS-type copper deposit.展开更多
The Tongyu copper deposit, located in the western part of the North Qinling Orogen, China, is one of several volcanic-hosted massive sulphide（VHMS） deposits with industrial value and is also a typical example of min...The Tongyu copper deposit, located in the western part of the North Qinling Orogen, China, is one of several volcanic-hosted massive sulphide（VHMS） deposits with industrial value and is also a typical example of mineralization related to the subduction and metallogenesis during the Caledonian orogeny. We conducted systematic lead-sulphur isotope geochemical analyses of the Tongyu deposit to understand the possible ore-forming material sources and tectonic settings. Twenty-six sulphide samples yielded clustered δ^34SCDT values of 1.13‰-3.36‰, average 2.22‰, and show a tower-type distribution,implying that the sulphur of the Tongyu copper deposit mainly originated from a mantle source. The Pb isotope compositions of sulphides（^206Pb/^204Pb = 17.59225-18.56354, average 18.32020; ^207Pb/^204Pb =15.51770-15.69381, average 15.66217; ^208Pb/^204Pb= 37.99969-39.06953, average 38.52722） are close to the values of the volcanic host rocks（^206Pb/^204PbPb= 18.10678-18.26293, average 18.21158; ^207Pb/^204PbPb =15.63196-15.68188, average 15.65345; ^208Pb/^204PbPb= 38.43676-38.56360, average 38.49171）, thus consistent with the Pb in ores and volcanic host rocks having been derived from a common source that was island-arc Pb related to oceanic crust subduction. The northward subduction of the Palaeo-Qinling oceanic crust triggered dehydration of the slab, which generated a large amount of high-oxygen-fugacity aqueous hydrothermal fluid. The fluid rose into the mantle wedge, activated and extracted metallogenic material and promoted partial melting of the mantle wedge. The magma and ore-forming fluid welled up and precipitated, finally forming the Tongyu VHMS copper deposit.展开更多
文摘目的探讨原发性中枢神经系统淋巴瘤(primary central nervous system lymphoma,PCNSL)的MRI表现,提高诊断水平。方法回顾性分析我院经病理证实的14例PCNSL患者的MRI资料。14例患者均进行MRI平扫及增强扫描,其中3例患者行MRS。由两名资深MRI诊断医师对MRI图像进行分析,包括病灶的部位、数目、信号特点、强化方式、瘤周水肿、囊变坏死、出血及MRS等。结果1)病灶数目14例患者中单发12例,多发2例,单发病例中有2例病变跨越两个脑叶,1例病变位于左侧小脑半球-小脑蚓部;2)病灶分布右额叶5个,左额叶5个,左顶叶2个,胼胝体2个,左侧大脑脚1个,左侧基底节2个,左右颞叶各1个,左侧小脑半球2个;3)信号特点等T110个,稍长/长T19个;等T28个,稍长/长T211个;DWI稍高信号8个,高信号11个;4)强化特点不均匀强化3例,明显均匀强化11例,软脑膜强化3例,2例多发病例中所有病灶均明显均匀强化;5)瘤周水肿重度水肿2个,中度水肿3个,轻度水肿14个;6)出血及囊变出血2个,囊变2个。结论增强、弥散加权成像联合瘤周水肿对PCNSL的诊断有重要价值,MRS对鉴别诊断有一定的作用。
文摘目的探讨3.0 T磁共振3D-T1-可变反转角快速自旋回波(Sampling Perfection with Application Optimized Contrasts Using Different Fip Angle Evolution,3D-T1-SPACE)增强序列评估大脑中动脉(Middle Cerebral Artery,MCA)粥样硬化患者受累血管的临床价值。方法分析46例单侧MCA粥样硬化性狭窄患者临床、影像资料,对比评估3D-T1-SPACE增强、三维时间飞跃法磁共振血管成像(Three Dimensional Time of Flight Magnetic Resonance Angiography,3D-TOF-MRA)在测量管腔狭窄及病变长度方面与数字减影血管造影(Digtial Subtraction Angiography,DSA)的一致性。结果相比DSA,3D-T1-SPACE增强在评估管腔狭窄方面的一致性优于3D-TOF-MRA(ICC=0.91、0.80),而两者在测量病变长度方面均高于DSA(P<0.001);DSA、3D-TOF-MRA显示管腔局部轻微凹陷可疑狭窄时,3D-T1-SPACE增强序列可有效检出管壁微小斑块。结论3D-T1-SPACE增强序列能有效评估MCA粥样硬化管腔狭窄、病变长度及斑块特征,可作为MCA粥样硬化患者常规无创诊断及随访评估手段。
基金jointly supported by the National Natural Science Foundation of China(Grant Nos.41272092,41421002 and 41072068)Program for Changjiang Scholars and Innovative Research Team in University(Grant IRT1281)+1 种基金Natural Science Basic Research Program of Shaanxi Province,China(Grant No.2013JZ013)Graduate Innovation Funds of Northwest University,China(Grant No.YZZ12006)
文摘Precise in situ zircon U-Pb dating and Lu-Hf isotopic measurement using an LA-ICP-MS system, whole-rock major and trace element geochemistry and Sr-Nd isotope geochemistry were conducted on the volcanic host rocks of the Tongyu copper deposit on the basis of further understanding of its geological characteristics. Three zircon samples from the volcanic host rocks yielded 206Pb/238 U weighted average ages ranging from 436±4 Ma to 440±5 Ma, which are statistically indistinguishable and coeval with the ca. 440 Ma northward subduction event of the Paleo-Qinling oceanic slab. The volcanic host rocks were products of magmatic differentiation that evolved from basalt to andesite to dacite to rhyolite, forming an integrated tholeiitic island arc volcanic rock suite. The primitive mantle-normalized trace element patterns for most samples show characteristics of island arc volcanic rocks, such as relative enrichment of LILE（e.g. Th, U, Pb and La） and depletion of HFSE（e.g. Nb, Ta, Ti, Zr and Hf）. Discrimination diagrams of Ta/Yb vs Th/Yb, Ta vs Th, Yb vs Th/Ta, Ta/Hf vs Th/Hf, Hf/3 vs Th vs Nb/16, La vs La/Nb and Nb vs Nb/Th all suggest that both the volcanic host rocks from the Tongyu copper deposit and the volcanic rocks from the regional Xieyuguan Group were formed in an island arc environment related to subduction of an oceanic slab. Values of ISr（0.703457 to 0.708218） and εNd（t）（-2 to 5.8） indicate that the source materials of volcanic rocks from the Tongyu copper deposit and the Xieyuguan Group originated from the metasomatised mantle wedge with possible crustal material assimilation. Most of the volcanic rock samples show good agreement with the values of typical island arc volcanic rocks in the ISr-εNd（t） diagram. The involvement of crustal-derived material in the magma of the volcanic rocks from the Tongyu copper deposit was also reflected in the zircon εHf（t） values, which range from-3.08 to 10.7, and the existence of inherited ancient xenocrystic zircon cores（2616±39 Ma and 1297±22 Ma）. The mineralization of the Tongyu copper deposit shows syn-volcanic characteristics such as layered orebodies interbedded with the volcanic rock strata, thus, the zircon U-Pb age of the volcanic host rocks can approximately represent the mineralization age of the Tongyu copper deposit. Both the Meigou pluton and the volcanic host rocks were formed during the ca. 440 Ma northward subduction of the Paleo-Qinling Ocean when high oxygen fugacity aqueous hydrothermal fluid released by dehydration of the slab and the overlying sediments fluxed into the mantle wedge, triggered partial melting of the mantle wedge, and activated and extracted Cu and other ore-forming elements. The magma and ore-bearing fluid upwelled and erupted, and consequently formed the island arc volcanic rock suite and the Tongyu VHMS-type copper deposit.
基金jointly supported by National Natural Science Foundation of China(Grant Nos.41421002,41272092,and 41030423)MOST Special Fund from the State Key Laboratory of Continental Dynamics,Northwest University,China
文摘The Tongyu copper deposit, located in the western part of the North Qinling Orogen, China, is one of several volcanic-hosted massive sulphide（VHMS） deposits with industrial value and is also a typical example of mineralization related to the subduction and metallogenesis during the Caledonian orogeny. We conducted systematic lead-sulphur isotope geochemical analyses of the Tongyu deposit to understand the possible ore-forming material sources and tectonic settings. Twenty-six sulphide samples yielded clustered δ^34SCDT values of 1.13‰-3.36‰, average 2.22‰, and show a tower-type distribution,implying that the sulphur of the Tongyu copper deposit mainly originated from a mantle source. The Pb isotope compositions of sulphides（^206Pb/^204Pb = 17.59225-18.56354, average 18.32020; ^207Pb/^204Pb =15.51770-15.69381, average 15.66217; ^208Pb/^204Pb= 37.99969-39.06953, average 38.52722） are close to the values of the volcanic host rocks（^206Pb/^204PbPb= 18.10678-18.26293, average 18.21158; ^207Pb/^204PbPb =15.63196-15.68188, average 15.65345; ^208Pb/^204PbPb= 38.43676-38.56360, average 38.49171）, thus consistent with the Pb in ores and volcanic host rocks having been derived from a common source that was island-arc Pb related to oceanic crust subduction. The northward subduction of the Palaeo-Qinling oceanic crust triggered dehydration of the slab, which generated a large amount of high-oxygen-fugacity aqueous hydrothermal fluid. The fluid rose into the mantle wedge, activated and extracted metallogenic material and promoted partial melting of the mantle wedge. The magma and ore-forming fluid welled up and precipitated, finally forming the Tongyu VHMS copper deposit.
