Integrating 40Ar-39Ar, 87Rb-87Sr and 147Sm-143Nd geochronology of authigenic illite to evaluate tectonic reactivation in an intraplate setting, central Australia

The Warburton-Cooper basins, central Australia, include a multitude of reactivated fracture-fault networks related to a complex, and poorly understood, tectonic evolution. We investigated authigenic illites from a granitic intrusion and sedimentary rocks associated with prominent structural features (Gidgealpa-Merrimelia-Innamincka Ridge and the Nappamerri Trough). These were analysed by 40Ar-39Ar, 87Rb-87Sr and 147Sm-143Nd geochronology to explore the thermal and tectonic histories of central Australian basins. The combined age data provide evidence for three major periods of fault reactivation throughout the Phanerozoic. While Carboniferous (323.3 ± 9.4 Ma) and Late Triassic ages (201.7 ± 9.3 Ma) derive from basin-wide hydrothermal circulation, Cretaceous ages (~128 to ~86 Ma) reflect episodic fluid flow events restricted to the synclinal Nappamerri Trough. Such events result from regional extensional tectonism derived from the transferral of far-field stresses to mechanically and thermally weakened regions of the Australian continent. Specifically, Cretaceous ages reflect continent-wide transmission of tensional stress from a > 2500 km long rifting event on the Eastern (and southern) Australian margin associated with break-up of Gondwana and opening of the Tasman Sea. By integrating 40Ar-39Ar, 87Rb-87Sr and 147Sm-143Nd dating, this study highlights the use of authigenic illite in temporally constraining the tectonic evolution of intracontinental basins that would otherwise remain unknown. Furthermore, combining Sr- and Ar-isotopic systems enables more accurate dating of authigenesis whilst significantly reducing geochemical pitfalls commonly associated with these radioisotopic dating methods.

Geocronologia (40Ar/39Ar e U-Pb), petrografia e litogeoquímica da intrusão alcalina do Marapicu RJ

A intrusão alcalina do Marapicu é uma intrusão localizada no maciço Marapicu-Gericinó-Mendanha situado na região metropolitana do Rio de Janeiro. Este maciço é formado por dois corpos alcalinos: Marapicu e Mendanha que fazem parte do lineamento magmático Poços de Caldas-Cabo Frio. Este lineamento inclui dezenas de corpos ígneos alcalinos de idade Cretácea com uma direção preferencial WNW-ESE. Os litotipos mais abundantes do Maciço Marapicu são representados por nefelina sienitos e sienitos de caráter plutônico, além de, fonolitos caracterizados por intrusões rasas geralmente em forma de diques. Além desses litotipos foram amostradas duas rochas com características químicas de magma parental (lamprófiro e fonolito tefrítico), porém, essas duas amostras não apresentam relação genética com as demais. Também foi amostrado um nefelina sienito que possui sodalita azul como feldspatóide, sendo assim, chamado de nefelina sodalita sienito. Entre os fonolitos coletados para esse trabalho, uma amostra apresenta granada melanita em sua assembleia mineralógica, e esta foi então denominada melanita fonolito. Quimicamente as rochas do Marapicu formam uma série alcalina predominantemente insaturada em sílica, miaskítica e metaluminosa. Dentro desta série se observam duas suítes sendo uma potássica (predominante) e outra sódica. A evolução química do corpo se deu por processo de cristalização fracionada com ou sem assimilação de crosta continental provavelmente dentro de uma fonte mantélica enriquecida. Duas idades de cristalização foram obtidas para o Maciço do Marapicu sendo uma idade 40Ar/39Ar de 80,46 0,58 Ma em hornblenda, e uma idade U-Pb em zircão bastante concordante de 78,0 2,1 Ma. Os dados apresentados aqui em conjunto com dados da literatura apontam para dois modelos geodinâmicos de geração dos corpos alcalinos do sudeste brasileiro, um considera a existência de uma pluma mantélica gerada na astenosfera, o outro tem por base a hipótese de flexura crustal e considera que a carga de sedimentos depositados na plataforma continental exerceria esforços que provocariam fraturas profundas permitindo a ascenção desses magmas. O presente trabalho vem para contribuir no entendimento do alojamento dos corpos alcalinos do sudeste brasileiro através do estudo especifico do Maciço Marapicu em conjunto com dados da literatura

多丝正比室的研制与25 MeV/u 40Ar + 93Nb反应中轻粒子的发射时间测量

本论文共由两部分组成。第一部分描述了多丝正比室的研制过程。第二部分研究了中能区25MeV/u ~(40)Ar + ~(93)Nb反应中轻粒子发射时间的测量。本论文所研制的多丝正比室灵敏面积为5cm * 5cm。阳极丝由10μm的镀金钨丝组成，丝与丝之间的间距为0.5mm。工作气体为正庚烷，采用感应信号重心读出方法。调试了工作气压在25Torr左右、工作电压～1400v条件下多丝室的工作状态，结果表明该工作条件下，多丝正比室并未工作于正比状态下，须适当增加工作电压和工作气压才能得到较好的位置分辨。并且提出进一步的改进建议。第二部分利用小相对角度内的两粒子关联测量，研究了中能区25MeV/u ~(40)Ar + ~(93)Nb反应中高激发核衰变产生的轻粒子的发射时标。轻粒子发射时间随能量的变化很大，从低能粒子的约500fm/c变化至高能粒子的50fm/c，表明高能粒子来自于热核的早期发射，包含有前平衡发射的粒子，而低能粒子来自于平衡热核的发射。随着入射能的升高和激发能的增加，热核的寿命及其发射时标变短。轻粒子时空演化表明，发射源的核物质密度对轻粒子关联函数的影响较大，尤其是对于发射时间较(τ ≤ 100fm/c)的高能粒子的关联函数，这一影响随着粒子能量降低而减弱。在发射时间较长(τ ≤ 200fm/c)时，这种影响几乎消失。另外随着实验室系角度的增加，平衡发射成分增加，相应地提取的轻粒子的发射时间变长。

30,35MeV/u 36,40Ar＋112,124Sn反应中热核性质同位旋效应的实验研究

针对①中能反应中同位旋自由度是否达到平衡，②同位旋自由度对几中不同方法测量的核温度是否有影响 这两个基本问题，设计了用30和35MeV/u ~(36,40)Ar轰击~(112,124)Sn反应的实验方案。得到如下结果：对于前角5°处的耗散弹核碎裂产物，丰中子同位素与稳定核的产额比随产物出射动能的增加而减小，而丰质子子同位素与稳定核的产额比随动能的增加而增加，呈现明显的剪刀差分布特性。随耗散时间的增大，产物的平均中质比逐渐由弹核的平均中质比向系统的平均中质比过渡。这个结果说明在该反应中，同位旋自由度没有达到完全平衡。而对于20°处的DIC产物，上述剪刀差分布特性变得更不明显，这是同位旋自由度由非平衡向平衡过渡的表现。后角轻粒子的能谱分析表明，初始热核的同位旋会影响斜率核温度的提取，由于丰中子轻粒子~6He在~(40)Ar + ~(112)Sn系统中的蒸发被抑制，相比~(40)Ar + ~(112)Sn而言，其蒸发比较容易发生在衰变链早期，因此提取的温度偏高，同样，丰质子轻粒子~3He的温度在~(40)Ar + ~(112)Sn中略高。但中后角的同位素产额分析表明，反应系统的同位旋对双同位素比核温度几乎没有影响。核温度作为热核的热力学量，是独立于测量方法的，这种不同的方法得出的差异主要来源于同位旋对衰变机制的影响。作为一个尝试，将中高能反应中的熵的提取推广到这个能区，发现两个系统的熵几乎一致。在量子统计模型框架下，考察核温度与熵的关系发现，~(40)Ar + ~(112)Sn反应的挤出时刻密度略高于~(40)Ar + ~(112)Sn。

35 A×MeV 40Ar + 159Tb/197Au 反应中高激发核性质与反应机制研究

中能重离子碰撞的反应机制及其形成的高激发核的性质研究是当前中能重离子核物理研究的重要领域。本文通过对35 MeV/u~(40)Ar+~(159)Tb/~(197)Au反应中出射的轻粒子、中等质量碎片(IMF)和复合核裂变碎片的符合测量，研究了中等质量碎片的发射机制、类靶核的形成机制及其裂变时标、复合核的温度与激发能以及两者之间的关系等。利用前角探测器组的测量对前角区出射的IMF的单举和关联数据进行了分析。由弹核碎裂理论中的Gozdhaber关系式拟合了类弹碎片的能谱，由此提取的弹核的动量分布约化宽度为σ_0 ≈ 100MevV/c。通过Gemini模拟与IMF-IMF关联数据的对比揭示出激发的类弹碎片的裂变是关联IMF的一个重要来源。由IMF与裂变碎片以及IMF与后角轻粒子的关联数据显示出，在前角区域，当IMF的能量低于10 MeV/u时，复合核的蒸发对较轻IMF有较大的贡献；当IMF能量在10-24 MeV/u的区域时，IMF能量与复合核平均速度以及激发能之间存在着很强的依赖关系，说明这些IMF主要来源与弹靶之间的耗散反应；当IMF的能量超过24 MeV/u后，IMF能量与复合核平均速度以及激发能之间没有关联或关联很弱，说明在弹核碎裂的同时，靶核也发生了碎裂，它们共同贡献出部分核子形成了"中速源"或"颈部"。通过对复合核裂变时出射的关联裂片以及后角轻带电粒子的测量，提取了复合核的激发能以及在不同激发能能下所对应的核温度。对于中心碰撞，Au靶形成了E~* = 4MeV/u、T_(init) = 7.1 MeV的热核，Tb靶形成了E~* = 4.7MeV/u、T_(init) = 7.7MeV的热核。对其量热曲线的研究显示出，在当前入射能下没有观测到原子核液气相变的特征。由类弹碎片（PLF)与类靶核两个裂片的关联数据，提取了类靶核裂变轴在反应平面内的转动角度，并由此计算出类靶核的、裂变时标。在对称裂变时，类靶核的寿命约5 * 10~(-20) s，在非对称裂变（η =0.6）时降为约1.7 * 10~(-21) S。同时我们认为类靶核的裂变存在两种机制，即动力学裂变和统计裂变，分别对应于裂变轴在反应平面内的非各相同性分别和各相同性分布。

25Mev/u~40Ar+~27Al、~58Ni、~115In在小角区产物的研究

重离子核反应机制的研究一直是人们关注的课题。用25MeV/u 40Ar的束流进行多种反应机制共存及其对碎片的贡献的研究，有助于我们更清楚地了解反应机制的演化和对放射性束流产额的预言。 实验中用25MeV/u40Ar的束流轰击115In、58Ni、27Al，这时对前方向6°、8.5°的碎片测量，发现它们的平行动量分布宽度满足Goldhaber关系式，碎裂部分提取的约化平行动量分布宽度σ0=54MeV/c，这比弹核碎裂部分的宽度要窄，说明转移反应比弹核碎裂受到相空间的严格限制更严格。转移反应主要是对弹核附近的碎片有贡献，当类弹碎片质量与弹核质量相差较大时，主要是弹核碎裂的贡献。对于弹核碎裂产物的最可几能量的提取，在实验能谱中拟合出碎片的最可几能量，对于接近弹核的碎片，我们利用外推法来确定碎裂部分的最可几能量，同时用实验提取的σ0值，拟合出碎裂能谱，从而将弹核碎裂和转移反应的贡献区分开来。 通过碎片同位素的测量，我们认碎片的同位素分布与靶核有一定的依赖关系，当靶核的N/Z值增加时，产物的N/Z也增加。弹核40Ar的N/Z为1.22，靶核的N/Z均大于1，所以产物N/Z的变化意味着系统由非平衡向平衡的演化，且在这一能区，重离子反应既有低能下一体耗散的特点，又有高能下核子-核子碰撞的特点，多种反应机制共存并竞争。

30Mev/u~40Ar+~natAg轻粒子与复杂碎片的测量

利用气体探测器和CsI望远镜探测器测量了30MeV/u 40Ar+natAg反应中出射的轻粒子、中等质量碎片和重碎片。中能区轻粒子和中等质量碎片的发射成分与角度和碰撞参数有关。在前角区粒子和碎片主要来自于弹核碎裂，其平行动量分布宽度满足Goldhaber公式。提取的动量分布约化宽度σ0≈76MeV/c；在后角区轻粒子和中等质量碎片主要来自于类靶平衡热核的蒸发。利用单源模型能很好地拟合其发射能谱，由α粒子能谱提取的核温度约为4.2MeV；同时利用He/Li同位素比的方法得到的核温度约为4.6MeV。

东南沿海火山碎屑岩40Ar/39Ar年代学研究

The Mesozoic pyroclastic rocks cover a vast coastal area in southeastern China, which is an important part of volcanic belt around Pacific Ocean. However, the previous dates for these rocks are confused and conflicted with each other, which have limited the further researches. It is difficult to date pyroclastic rocks, for almost all the dating methods, due to the multiple sources during their formation. Single crystal laser probe 40Ar/39Ar method is a powerful means to date pyroclastic rocks with complex sources. By distinguishing the xenocrysts and altered materials, Singe crystal total fusions of CO2 lasing on the sanidine separates could yield rational 40Ar/39Ar results and distinguish their sources. Timing on formations of the Moshishan Group, after avoiding the exotic and altered grains by lasing on the single sanidine separate, was reported in this study. 40Ar/39Ar incremental heating results of Cement part of the pyroclastic rocks show that the age spectrums are too complex to interpret for geological significance because of the alteration and 39Ar recoil. Incremental heating on K-feldspar separate from pyroclastic rocks give reliable data. Combining 40Ar/39Ar incremental heating ages and laser total fusion ages, we suggest the age was 125Ma-120Ma for Dashuang Fm, 120-119 Ma for Gaowu Fm, 119-114Ma for Xishantou Fm, 114-112Ma for Chawan Fm and 112-110Ma for Jiuliping Fm. The most intense period of volcanic activity in eastern Zhejiang Province was at about 120Ma. These new ages are much younger than the previous ones, suggesting that these thick volcanic formations had been formed in very short durations.

云南武定迤腊厂铜矿含矿石英脉^40Ar-^39Ar年龄及其意义

对武定迤腊厂铜矿成矿期石英进行了^40Ar-^39Ar同位素年龄测定，得到马鞍形年龄谱，坪年龄为(784．25±0．95)Ms，等时线年龄为(783．93±8．59)Ma。地质特征研究表明：该矿床后期改造作用明显，并非同生沉积或成岩作用早期成矿，而与晋宁期Rodina大陆裂解有关。武定迤腊厂铜矿的形成可能是在Rodinia大陆裂解时，从深部带来大量成矿物质，改造成岩时期初始的矿化，形成矿床的叠加富集和最终定位，晋宁．澄江期是该矿床的主成矿期。

四川盐边高家村镁铁-超镁铁质杂岩体的形成时代: 单颗粒锆石U-Pb和角闪石40Ar/39Ar年代学制约

四川盐边高家村镁铁-超镁铁质杂岩体是一个分异良好的似层状侵入体, 该岩体可以分为两个堆积旋回. 对高家村杂岩体主体岩相的角闪辉长岩进行系统的单颗粒锆石U-Pb定年以及单矿物角闪石40Ar/39Ar定年的研究, 表明高家村杂岩体的主体岩相形成年龄为840±5 Ma. 对“盐边蛇绿岩”的提法提出了质疑, 认为高家村杂岩体的形成很可能与Rodinia超级大陆下的一个超级地幔柱活动有关. 以上的研究成果有助于重新认识盐边地区新元古代构造演化特征.