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lithosphere types in North China:Evidence from geology and geophysics

Science China Earth sciences 2005年第11期48卷 1809-1827页

作者： qiu ruizhao1,2, deng jinfu3. zhou su3. li jinfa4. xiao qinghui1,5, wu zongxu6 & liu cui3.1. institute of geology, chinese academy of geological sciences,{4., China 2. Development and Research Center, China geological survey,{4., China 3. China University of Geosciences, beijing 100083, China 4. China University of Geosciences, wuhan 4.0074. China 5. Information Center of Ministry of Land and Resources, beijing 100812, China 6. institute of {14., State Seismological Bureau, beijing 100029, China 1. institute of geology Chinese Academy of Geological Sciences 100037 Beijing China 2. Development and Research Center China Geological Survey 100037 Beijing China 3. China University of Geosciences 100083 Beijing China 4. China University of Geosciences 430074 Wuhan China 5. Information Center of Ministry of Land and Resources 100812 Beijing China 6. institute of geology State Seismological Bureau 100029 Beijing China

On the basis of the characteristics of geology and geophysics in North China, three types of lithosphere, namely, the cratonic, the orogenic and the rift lithospheres can be classified. In terms of petrological method (based on the information from Precambrian rock assemblages, igneous activities, deep-seated enclaves, etc.) and the relationship between seismic velocity and rock compositions, the crust-mantle petrological and chemical structure models can be set up. Researching results indicate that the geology and geophysics of North China platform bears the similar characteristics in comparison with those of the global typical cratons. The Eerduosi(Ordos) block located in the west of the North China Platform is a remnant of cratonic lithosphere after the North China platform had undergone “activation” in Mesozoic and “reconstruction” in Cenozoic times. The continental crust consists mainly of TTG rock assemblage while the subcontinental lithosphere mantle mainly consists of strongly depleted harzburgite. The craton was finally formed in late Archaean and early Proterozoic, and has been kept in stability up to present; its crustal-mantle petrological structures of lithosphere can be set up as a reference for the study of North China craton and even Sino-Korean craton. In the Mesozoic period, the middle and east areas of North China platform were activated in the Yanshanian orogenic process, the continental crust was reformed by material and heat-transfer of convective mantle and the original crustal TTG component was reconstructed to be granitic crust, and the subcontinental lithosphere man- tle was replaced by the Yanshanian harzburgite-lherzolite. The Yanshan-Taihang Mountains were the remnants of orogenic lithosphere after the rifting in eastern North China in Cenozoic. The present thickness of continental crust and lithosphere in the Yanshan-Taihang Mountains is not equal to their thickness during the Yanshanian orogenic movement because they had undergone the

关键词： lithospheric types,evidence of geology and geophysics,crust-mantle petrological structure,deep process

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Amplitude analysis of the decays D^(0)→π^(+)π^(−)π^(+)π^(−)and D^(0)→π^(+)π^(−)π^(0)π^(0)

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chinese Physics C 2024年第8期48卷 6-33页

作者： M.Ablikim M.N.Achasov P.Adlarson O.Afedulidis X.C.Ai R.Aliberti A.Amoroso Q.An Y.Bai O.Bakina I.Balossino Y.Ban H.-R.Bao V.Batozskaya K.Begzsuren N.Berger M.Berlowski M.Bertani D.Bettoni F.Bianchi E.Bianco A.Bortone I.Boyko R.A.Briere A.Brueggemann H.Cai X.Cai A.Calcaterra G.F.Cao N.Cao S.A.Cetin J.F.Chang W.L.Chang G.R.Che G.Chelkov C.Chen C.H.Chen Chao Chen G.Chen H.S.Chen M.L.Chen S.J.Chen S.L.Chen S.M.Chen T.Chen X.R.Chen X.T.Chen Y.B.Chen Y.Q.Chen Z.J.Chen Z.Y.Chen S.K.Choi X.Chu G.Cibinetto F.Cossio J.J.{4. H.L.Dai J.P.Dai A.Dbeyssi R.E.de Boer D.Dedovich C.Q.deng Z.Y.deng A.Denig I.Denysenko M.Destefanis F.De Mori B.Fang S.S.Fang W.X.Fang Y.Fang Y.Q.Fang R.Farinelli L.Fava F.Feldbauer G.Felici C.Q.Feng J.H.Feng Y.T.Feng K.Fischer M.Fritsch C.D.Fu J.L.Fu Y.W.Fu H.Gao Y.N.Gao Yang Gao S.Garbolino I.Garzia P.T.Ge Z.W.Ge C.Geng E.M.Gersabeck B.Ding X.X.Ding Y.Ding Y.Ding J.Dong L.Y.Dong M.Y.Dong X.Dong M.C.Du S.X.Du Z.H.Duan P.Egorov Y.H.Fan J.Fang JA.Gilman K.Goetzen L.Gong W.X.Gong W.Gradl S.Gramigna M.Greco M.H.Gu Y.T.Gu C.Y.Guan Z.L.Guan A.Q.Guo L.B.Guo M.J.Guo R.P.Guo Y.P.Guo A.Guskov J.Gutierrez K.L.Han T.T.Han X.Q.Hao F.A.Harris K.K.He K.L.He F.H.Heinsius C.H.Heinz Y.K.Heng C.Herold T.Holtmann P.C.Hong G.Y.Hou X.T.Hou Y.R.Hou Z.L.Hou B.Y.Hu H.M.Hu J.F.Hu T.Hu Y.Hu G.S.Huang K.X.Huang L.Q.Huang X.T.Huang Y.P.Huang T.Hussain F.H\"olzken N.H\"usken N.in der Wiesche M.Irshad J.Jackson S.Janchiv J.H.Jeong Q.Ji Q.P.Ji W.Ji X.B.Ji X.L.Ji Y.Y.Ji X.Q.Jia Z.K.Jia D.Jiang H.B.Jiang P.C.Jiang S.S.Jiang T.J.Jiang X.S.Jiang Y.Jiang J.B.Jiao J.K.Jiao Z.Jiao S.Jin Y.Jin M.Q.Jing X.M.Jing T.Johansson S.Kabana N.Kalantar-Nayestanaki X.L.Kang X.S.Kang M.Kavatsyuk B.C.Ke V.Khachatryan A.Khoukaz R.Kiuchi O.B.Kolcu B.Kopf M.Kuessner X.Kui A.Kupsc W.K\"uhn J.J.Lane P.Larin L.Lavezzi T.T.Lei Z.H.Lei H.Leithoff M.Lellmann T.Lenz C.li C.li C.H.li Cheng li D.M.li F.li G.li H.li H.B.li H.J.li H.N.li Hui li J.R.li J.S.li K.li L.J.li L.K.li Lei li M.H.li P.R.li Q.M.li Q.X.li R.li S.X.li T.li W.D.li W.G.li X.li X.H.li X.L.li X.Y.li Y institute of High Energy Physics Chinese Academy of SciencesBeijing 100049China Beihang University Beijing 100191China Bochum Ruhr-University D-44780 BochumGermany Budker institute of Nuclear Physics SB RAS(BINP) Novosibirsk 630090Russia Carnegie Mellon University PittsburghPennsylvania 15213USA Central China Normal University Wuhan 430079China Central South University Changsha 410083China China Center of Advanced Science and Technology Beijing 100190China China University of Geosciences Wuhan 430074China Chung-Ang University Seoul06974Republic of Korea COMSATS University Islamabad Lahore CampusDefence RoadOff Raiwind Road54000 LahorePakistan Fudan University Shanghai 200433China GSI Helmholtzcentre for Heavy Ion Research GmbH D-64291 DarmstadtGermany Guangxi Normal University Guilin 541004China Guangxi University Nanning 530004China Hangzhou Normal University Hangzhou 310036China Hebei University Baoding 071002China Helmholtz institute Mainz Staudinger Weg 18D-55099 MainzGermany Henan Normal University Xinxiang 453007China Henan University Kaifeng 475004China Henan University of Science and Technology Luoyang 471003China Henan University of Technology Zhengzhou 450001China Huangshan College Huangshan 245000China Hunan Normal University Changsha 410081China Hunan University Changsha 410082China Indian institute of Technology Madras Chennai 600036India Indiana University BloomingtonIndiana 47405USA INFN Laboratori Nazionali di Frascati INFN Laboratori Nazionali di FrascatiI-00044FrascatiItaly INFN Laboratori Nazionali di Frascati INFN Sezione di PerugiaI-06100PerugiaItaly INFN Laboratori Nazionali di Frascati University of PerugiaI-06100PerugiaItaly INFN Sezione di Ferrara INFN Sezione di FerraraI-44122FerraraItaly INFN Sezione di Ferrara University of FerraraI-44122FerraraItaly Inner Mongolia University Hohhot 010021China institute of Modern Physics Lanzhou 730000China institute of Physics and Technology Peace Avenue 54BUlaanbaatar 13330Mongolia Instituto de A

Using e^(+)e^(−)annihilation data corresponding to an integrated luminosity of 2.93 fb^(−1)taken at the center-of-mass energy√s=3.773 GeV with the BESIII detector,a joint amplitude analysis is performed on the decays D^(0)→π^(+)π^(−)π^(+)π^(−)and D^(0)→π^(+)π^(−)π^(0)π^(0)(non-η).The fit fractions of individual components are obtained,and large interferences among the dominant components of the decays D^(0)→a_(1)(1260)π,D^(0)→π(1300)π,D^(0)→ρ(770)ρ(770),and D^(0)→2(ππ)_(S)are observed in both *** the obtained amplitude model,the CP-even fractions of D^(0)→π^(+)π^(−)π^(+)π^(−)and D^(0)→π^(+)π^(−)π^(0)π^(0)(non-η)are determined to be(75.2±1.1_(stat).±1.5_(syst.))%and(68.9±1.5_(stat).±2.4.(syst.))%,*** branching fractions of D^(0)→π^(+)π^(−)π^(+)π^(−)and D^(0)→π^(+)π^(−)π^(0)π^(0)(non-η)are measured to be(0.688±0.010_(stat.)±0.010_(syst.))%and(0.951±0.025_(stat.)±0.021_(syst.))%,*** amplitude analysis provides an important model for the binning strategy in measuring the strong phase parameters of D^(0)→4.when used to determine the CKM angleγ(ϕ_(3))via the B^(−)→DK^(−)decay.

关键词： BESIII D^(0)meson decays amplitude analysis CP-even fraction

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广西壮族自治区8009例妇科恶性肿瘤住院患者的构成特点及变化趋势

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中华妇产科杂志 2007年第1期42卷 22-25页

作者：黄薇李力余冬青黄英兰刘燕陈心秋唐步坚徐红马刚董林红李廉邱映白桦农文政李立曾定元蒋福彦兰鹰叶元唐雄志王丹霞黎惠珍潘燕波莫爱旭吴笑彦雷志英周国萍刘翠苏庆红广西医科大学附属肿瘤医院妇瘤科南宁530021 广西医科大学第一附属医院妇产科南宁530021 广西壮族自治区人民医院妇科广西中医学院第一附属医院妇科南宁市第一人民医院妇产科南宁市第二人民医院妇产科广西壮族自治区妇幼保健医院妇科广西壮族自治区民族医院妇产科广西壮族自治区柳州市人民医院妇产科广西壮族自治区柳州市工人医院妇产科广西壮族自治区柳州市肿瘤医院妇瘤科广西壮族自治区柳州地区人民医院妇产科桂林医学院附属医院妇产科桂林市人民医院妇产科广西壮族自治区北海市第一人民医院妇产科广西壮族自治区北海市人民医院妇产科广西壮族自治区河池市第一人民医院妇产科广西壮族自治区河池市人民医院妇产科广西壮族自治区百色市人民医院妇产科右江民族医学院附属医院妇产科广西壮族自治区玉林市第一人民医院妇产科广西壮族自治区玉林市红十字会医院妇产科广西壮族自治区梧州市工人医院妇产科

目的了解广西壮族自治区近20年间妇科恶性肿瘤住院患者的构成特点及变化趋势。方法对1985—2004.间广西壮族自治区23家医院收治的8009例妇科恶性肿瘤患者的临床资料进行统计分析。结果(1)构成比:妇科恶性肿瘤中,构成比排在前4.的分别... 详细信息

目的了解广西壮族自治区近20年间妇科恶性肿瘤住院患者的构成特点及变化趋势。方法对1985—2004.间广西壮族自治区23家医院收治的8009例妇科恶性肿瘤患者的临床资料进行统计分析。结果(1)构成比:妇科恶性肿瘤中,构成比排在前4.的分别是宫颈癌、卵巢恶性肿瘤、子宫内膜癌、恶性滋养细胞肿瘤。其中,1985—1989年、2000—2004.宫颈癌住院患者的构成比呈上升的趋势,从17.4.%上升到4..25%,两者比较,差异有统计学意义(P69%下降到7.34.,两者比较,差异有统计学意义(P0.05)。(2)好发年龄:近10年,宫颈癌的发病年龄明显前移,从≥60岁前移到4.岁,两者比较,差异有统计意义(P5)。(3)地域和职业分布:前10年宫颈癌患者主要集中于城市,构成比为67.1%;后10年却逐渐向农村转移,农村宫颈癌患者构成比达52.6%。(4.手术病理分期或临床分期:妇科恶性肿瘤患者就诊时大多数已经处于Ⅱ、Ⅲ、Ⅳ期,中晚期(Ⅲ、Ⅳ期)的构成比多在60%以上。结论(1)应重点加强对宫颈癌的普查防治工作,同时也要加大对其他妇科肿瘤的防治力度。(2)加大对相应肿瘤标志物、新的诊治方法的发现和研究力度,提高早期诊治率。

关键词：生殖器肿瘤,女(雌)性宫颈肿瘤流行病学方法

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