Laser step-heating ^40Ar/^39Ar dating on young volcanic rocks

An attempt was made to use CO_2 laser step-heating method to date the late Pleistocene basaltic groundmass (DF-2) from Tengchong volcanic field. Among the fourteen heating steps, ten define a good inverse isochron (MSWD = 1.4) with an age of 32.2 ± 7.1 ka (2 σ).The inverse isochron also shows that the initial argon isotopic ratio is 297.1±2.0 (2σ) which is the same as the atmospheric argon at the 2σ error level. Study indicates that it is a useful means to date young volcanic groundmass with low K content by using CO_2 laser step-heating ~(40)Ar/~(39)Ar method.     

ISEA reversed event in the Cretaceous Normal Super-chron （CNS）： ^40Ar／^39Ar dating and paleomagnetic results

ThegeomagneticfieldwasfoundtobeofnormalpolarityforalongtimeduringtheCretaceousbyHelsleyandSteiner[1]andthiswaslaternamedasCretaceousNormalSuperchron(CNS)[2].TheCNSlastedalmost37Ma(120—83Ma).Severalabnormalgeologicalevents,suchasanoceanicanoxicevent,alargenumberofvol-canismandglobalclimaticwarmingduringtheCNShavebeenreported[3—11].Thishasledtomanyquestionsbeingraised.IsittruethattheEarthsmagneticfielddidnotreverseatallintheCNS?Ifitdidreverse,howmanytimesandwhendidthishappen?Istherea…     

Experiment of the ~(40)Ar/~(39)Ar dating of diagenetic illite in gas reservoirs

40Ar/39Ar dating of diagenetic illite has been performed to investigate gas reservoirs in the Sulige Gas Field of the northern Ordos Basin. A series of technical challenges were confronted, including illite purification, Ar recoil loss, and separation of diagenetic illite from detrital illite. Mineral growth ages for diagenetic illite were obtained by this experiment, from which the age of gas emplacement was deduced to be later than 169 Ma.     

40Ar/39Ar同位素体系及其在地学上的应用

40Ar/39Ar同位素体系大体经历了3个技术阶段常规 40Ar/39Ar定年技术、40Ar/39Ar分步加热定年技术和40Ar/39Ar激光显微探针定年技术.研究表明可以通过大气中40Ar/39Ar比值随时间的变化窥探地球去气作用的时间和强度;40Ar/39Ar法不仅有助于研究岩浆冷却过程和花岗岩侵位机制等岩浆动力学的历史和壳幔演化,而且对研究热液成矿年龄也是很有效方法之一;在一定的地质条件下,沉积地层时代越老,40Ar/39Ar值越高;当今40Ar/39Ar年代法已为全球环境演变研究提供了一种强有力的工具.     

用^211At和^131I标记蛋白质的研究

报道了砹—211和碘—131标记蛋白质的方法.通过过氧化氢或氯胺T直接氧化制备,使用凝胶色谱从反应产物中分离标记蛋白质,相对法比较放射性计数测定标记产率,过氧化氢适用于~(211)At标记蛋白质,氯胺T有利于~(131)I标记蛋白质.8次实验的结果表明,用过氧化氢氧化标记的~(211)At牛血清白蛋白产率96.4％,氯胺T氧化标记的~(?)I牛血清白蛋白产率66.1％.间接法标记蛋白质,放射性核素~(211)At同对氨基苯甲酸反应获得对—~(211)At—苯甲酸,经乙醚萃取和高效液体色谱分离,然后再偶联到免疫球蛋白或牛血清白蛋白上。动物实验结果表明,此种结合的标记蛋白质在体内稳定,标记率不低于初始~(211)At放射性活度的40%.     

Lasing on pyroclastic rocks:A case study of ~(40)Ar/~(39)Ar dating on Moshishan Group,eastern Zhejiang Province

It is difficult to date pyroclastic rocks,for almost all the dating methods,due to the multiple sources during their formation.40Ar/39Ar incremental heating results on groundmass selected from the samples show that the age spectra are meaningless geologically.However,singe crystal total fusions of CO2 lasing on the sanidine separates could yield rational 40Ar/39Ar results and distinguish their sources in this study.Timing on three formations of the Moshishan Group,after avoiding the exotic and altered grains by lasing on the single sanidine separate,was reported in this paper.The lowermost portion of the Chawan Formation gives an age of 113.7±0.3 Ma;the lower part of the Xishantou Formation was formed 116.4±0.4 Ma ago and the bottom of the Gaowu Formation took its shape at 118.4±0.4 Ma.These new ages are much younger than the previous ones,suggesting that these thick volcanic formations had been formed in very short durations.     

14.6MeV中子的^56Fe（n,p）^56Mn反应截面

本文评价了14.6MeV 中子的~(56)Fe(n,p)~(56)Mn 反应截面,评价值为(109.6±0.6)×10~(-27)cm~2。又报告了利用我校400kV 高压倍加器 D-T 中子源的测量工作。中子通量密度是用~(27)Al(n,p)~(27)Mg 和~(63)Cu(n,2n)~(62)Cu 反应截面进行刻度的.~(56)Mn 的γ放射性是利用 NaI谱仪和高纯锗多道谱仪进行测量的。经修正后的测量结果为(110.7±1.9)×10~(-27)cm~2,在误差围内与评价值相符。     

华南武夷山早古生代构造事件的^40Ar／^39Ar同位素年龄研究

华南武夷山地区广泛发育一套强烈韧性剪切变形的中、高级变质岩系,其新生矿物白云母非常普遍.对武夷山南麓政和县蝴碟街大理岩和北麓弋阳县慈竹片麻状花岗岩中的动力变质矿物白云母进行40Ar/39Ar法同位素测年,分别获得391±3Ma和421±8Ma的坪年龄值,以及385±5Ma和422±6Ma的等时线年龄值,时代相当于志留纪末到泥盆纪初.结合地质证据,认为武夷山地区存在过一期早古生代沉积作用和早古生代末期的构造热事件.至少有一期的强烈韧性剪切变形和糜棱岩化作用是该构造事件所导致     

用MS-X_α方法研究(CrO_4)~(5-)的电子能级

本文采用了自旋极化MS-X_α方法,计算了铬离子(CrO_4)~(5-)的电子结构,给出了单电子本征值、本征函数和自旋极化分裂。用过渡态理论确定了基态组态,计算了部分光学跃迁和电荷转移跃迁的能量,并研究了配位体距离的影响。     

厦门地区~7Be和~(210)Pb的大气沉降通量

7Be和210Pb是大气中天然存在的放射性核素.本文测定了2001年8月至2002年8月间厦门地区7Be和210Pb大气沉降通量,平均值分别为1.90和0.41Bqm-2d-1.对7Be和210Pb的沉降特征及其影响因素进行了探讨,表明降雨是影响沉降通量的主要因素,两个核素的沉降通量之间存在较好线性相关性.     

14Mev中子的~(64)Zn(n,2n)~(63)Zn反应截面测量

本文用活化法分别以~(56)Fe(n,P)~(56)Mn和~(63)Cu(n,2n)~(62)Cu反应截面为标准,测量了14.61Mev中子的~(64)Zn(n,2n)~(63)Zn反应截面,其值分别为190.1±5.3mb和196.3±7.7mb。又以~(27)Al(n,P)~(27)Mg反应截面为标准,测量了14.13Mev、14.61Mev和14.85Mev三个能点的~(64)Zn(n,2n)~(63)Zn反应戡面,其值分别为116.0±8.7mb、189.4±14.2mb和197.2±14.8mb。活化生成核发射的γ射线用高纯锗(HPGc)γ谱议进行测量。     

杂交水稻苗期生长优势与~(32)P、~(14)C在分蘖的分布

试验杂交水稻的分蘖数量除L301A×R29比不育系和常规高产品种“双桂36”较少外,D优63、D优64、青优中、协优64、威优64、威优35和华优63分别比其亲本和对照品种多,表现正显性超亲优势.青优中、协优64、威优64、威优35、华优63和D优63的分蘖数与~(32)P在分蘖中的分布(％)呈正相关.D优64、L301A×R29不呈正相关.D优63、D优64、协优64的分蘖数与~(14)C—同化物在化分蘖的分布(％)呈正相关,青优中、威优64、威优35华优63和L301A×R29不呈正相关.D优63、D优64、协优64和华优63的单苗干物重高于它们的亲本和对照品种.青优中、协优64、华优63、D优63、D优64的苗高也分别比其亲本和对照品种高.本文还讨论了杂交稻苗期生长优势、~(32)P和~(14)C在分蘖中的分布(％)与谷粒产量的关系.     

Dating of sediment-hosted disseminated-type gold deposit by using ~(40)Ar/~(39)Ar laser probe: A case study of Changkeng large-scale gold deposit, China

Ore-forming age is one of the most important data in studying the genesis of mineral deposits. Dating of sedi-ment-hosted disseminated-type gold deposits, which areone of the most important types of gold deposits in theworld, is always a difficult task for ore geologists. Themajor reason is that most of the ores in this type deposit are of various siliceous and are composed of extremely fine-grained minerals, thus it will be very difficult to de-termine their ages by using conventional isotopi…     

~(168)Lu高自旋带退激的观测

通过束流能量为94MeV的熔合蒸发反应154Sm(19F,5n)168Lu布居了双奇核168Lu的高自旋态,发现一条新转动带,将其指定为建立在π7/2+[404]υ5/2-[523]基态上的转动带,并发现了π7/2+[404]υ5/2+[642]和π9/2-[514]υ5/2+[642]转动带同低激发态间的连接关系,确定了转动带的自旋.