U-Pb zircon age for the Nanhua-Sinian boundary

China Commission on Stratigraphy approved a tripartite classification of the Neoproterozoic in 2001 . Top of the new system was assigned to the base of the Doushan tuo Formation, the glacier-related strata were separated from the pro-Sinian System and named the Nanhua System, in which Nanhua is after the term of “the Nanhua great glaciations” proposed by Prof. Liu. In March 2004,     

Identification of Mesoproterozoic zircons in a Triassic dolerite from the Liaodong Peninsula,Northeast China

Evolution of mantle and crust in all blocks of China and their relationship with the surrounding blocks are re-lated to amalgamation and breakup of the supercontinents. Studies on the Mesoproterozoic Grenvillian orogeny and the configuration of Neoproterozoic Rodinia provide the most important advances to the ideas of continental crustal growth and configuration of plates[1,2]. Recent studies show that there are geological records of assembly and breakup of Rodinia in the Cathaysia and Yang…     

Zircon U-Pb SHRIMP dating for the volcanic rocks of the Xiong’er Group: Constraints on the initial formation age of the cover of the North China Craton

The volcanic rocks of the Xiong‘er Group occur widely in the southern part of the North China Craton, which mark the beginning of the cover in the southern part of the North China Craton. The age of the volcanic rocks is thus crucial to understand the tectonic regime and evolutionary history of the North China Craton in the Proterozoic age. Zircons from five volcanic rocks and intrusions were dated by U-Pb SHRIMP method. The results indicate that the Xiong‘er Group formed in 1.80--1.75 Ga of Paleo-Proterozoic. Since the Xiong‘er Group formed earlier than the Changcheng System, the earliest rocks in the Changcheng System is therefore assumed to be formed in 1.75 Ga. A thermal-tectonic event of ca. 1.84 Ga is indicated by new zircon U-Pb SHRIMP ages in the southern part of the North China Craton. The volcanic rocks of the Xiong‘er Group thus represent the initial magmatism of the Paleo-Proterozoic breakup of the North China Craton. Numerous inherited zircons in the volcanic rocks mainly formed in ～2.20 Ga, indicating that the source magma of the volcanic rocks may be derived from the ～2.20 Ga crust, or from a mantle magma with significant contamination of the ～2.20 Ga crust.     

Synthesis and characterization of organometallic macrocyclic rhodium (Ⅲ) complex with pyrazine ligands

The synthesis and structure research of organometal-lic macrocyclic complexes has been a very active field of modern chemistry [1—3]. In this field, Pd2+, Pt2+ complexes were first used as the building block, connected by het-erocyclic ligands, to construct metal macrocyclic com-pound[4,5]. The fac-Re(CO)5X (X = Cl, Br) fragment, for example, was shown to be a versatile building block for the synthesis of metallamacrocycles[6]. Some of this kind of molecule have been found applications in…     

黑龙江富饶组上段凝灰岩的SHRIMP锆石U-Pb年龄:一个最接近白垩系/第三系界线的年龄

白垩系和第三系(K/T)界线时期发生了显生宙最后一次大规模的生物绝灭和劫后复苏．自Alvarez等人根据UT界线的Ir异常提出生物大绝灭的小行星撞击假说后,K/T界线的精确时代、重大地质事件和生物大灭绝及其内在联系一直受到国际学术界的极大关注．K／T界限时期(约65Ma)的冲击石英和微玻球粒的广泛分布以及在墨西哥尤卡坦半岛发现同时代的Chicxulub陨石坑,使得撞击说得到了学术界越来越广泛的赞同．然而,另一些研究人员则认为由地幔柱引发的大规模火山岩喷发、地幔去气,     

高效非线性有机材料MHBA单晶的光学性能研究

我们利用分子工程法,设计、探索出了一种新型有机非线性光学材料三—甲基四—羟基苯甲醛。本文对MHBA单晶的结构特点、红外到紫外光透过率、光损伤阀值及其折射率变化等光学性能进行了全面研究。 三—甲氧基四—羟基苯甲醛,简称MHBA,分子式为C_6H_8O_3。利用改进的Hobden育     

BSCCO超导单晶的正电子湮没研究

一、引言 正电子是研究固体电子结构,固体缺陷和相变的灵敏探针。对超导体而言,BCS理论预言,Cooper对的形成导致k空间占据态的重新分布,从而引起费米面的模糊。理论预计费米面的模糊将使超导态的正电子寿命增加,湮没辐射Dopper展宽能谱的线形参数S下降。