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Kong Gao Guanghai Shi Meili Wang Gen Xie Jian Wang Xiaochong Zhang Ting Fang Weiyan Lei Yan Liu 《地学前缘(英文版)》2019,10(4):1597-1612
The Tashisayi nephrite deposit is located in South Altyn Tagh.in Qiemo County,Xinjiang Province,northwest China.It is a recent discovery in the vast,well-known Kunlun-Altyn nephrite belt distributed along the south of the Tarim Basin,producing more than half of the nephrite from the whole belt in 2017.Field investigations revealed that it is a dolomitic marble-related(D-type)nephrite deposit,but little is known about its age of formation and relationships between the granites and marble.Here we report field investigations,petrography of the neph rite,as well as petrography,geochemistry,geochronology of the zoisite-quartz altered intrusive rock and adjacent granites.An A-type granite is identified with a SHRIMP U-Pb zircon age of 926± 7 Ma,suggesting it was emplaced in an extensional tectonic environment at that time.The altered intrusive rock has a cluster of U-Pb zircon age of 433± 10 Ma.with similar trace element features to the A-type granite,suggesting it was formed in an extensional regime at this later time.Nephrite formed because of the metasomatism of dolomite marble by hydrothermal fluids.It is inferred that Ca~(2+) was released from the dolomitic marble by metasomatism forming Ca-rich fluids,which caused alteration of both the intrusive rocks(6.00-8.22 wt.% CaO)and granite(1.76-3.68 wt.% CaO)near the nephrite ore bodies.It is also inferred that Fe2+ from the granite migrated towards the dolomite marble.The fluids gave rise to the formation of Ca-minerals.such as zoisite,in the nephrite and altered intrusive rock,and epidote in the granite.Based on the contact relationships.similarity in hydrothermal processes,and consumption of Ca~(2+),the Tashisayi nephrite is considered to have formed at the same time as the alteration of the intrusive rocks,i.e.~433 Ma.The geochronological similarity(~926 Ma.433 Ma)of South Altyn and North Qaidam may suggest that tectonically they belong to one single complex in the past,which was offset by the Altyn Tagh fault(ATF).The similar formation ages of the nephrites from Altyn Tagh(433 Ma)and the previously studied areas of West Kunlun(378-441 Ma)and East Kunlun(416 Ma)indicate that these nephrites formed during the closure of Proto-Tethys and in the accompanving post-collisional.extensional environment. 相似文献
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ZHAO Changyi DU Meili SHAO Longyi CHEN Jianping CHENG Kerning HE ZhonghuaResearch Institute of Petroleum Exploration Development China National Petroleum Corporation Xueyuan Rd. Beijing Beijing Graduate School of China University of Mining Technology Xueyuan Rd. Beijing 《《地质学报》英文版》1998,72(2)
This paper discusses the enviromental characteristics of carbonaceous mudstone and mudstone (coal-measure mudstone in short) of the Early and Middle Jurassic in the Turpan-Hami basin, which were formed in swamps. Through the organic facies study of the coal-measure mudstone in this area, the authors clarify that the flowing-water swamp is the most advanced organic facies belt. Furthermore, according to the practical materials of coal-measure mudstone in the area and with the evaluation criteria of lacustrine mudstone in the past, the authors have established the integrated symbol systems from the abundance of organic matter and the type of organic matter, which can be used in the source rock evaluation of the coal-measure mudstone. 相似文献
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基于RUSLE的广东南岭土壤侵蚀敏感性研究 总被引:2,自引:0,他引:2
基于修正的通用水土流失方程RUSLE和GIS技术,分析了影响土壤侵蚀敏感性的降雨侵蚀力因子、土壤可蚀性因子、坡度坡长因子以及植被覆盖与管理因子,并生成单要素敏感性评价图,在此基础上,评价研究区土壤侵蚀敏感性,探讨不同土壤侵蚀敏感性的分布规律及其主导因子的空间分异特征。结果表明:降雨侵蚀力因子的变化范围为8 181.52~14 621.56(MJ·mm)/(hm2·h·a),土壤可蚀性因子为0.146~0.238(t·hm2·h)/(hm2·MJ·mm),坡度坡长因子为0~612.615,植被覆盖与管理因子为0.101~1.183,土壤侵蚀的最大值和平均值分别为7 016.44和137.69 t/(km2·a),土壤侵蚀敏感性以低度敏感和较低敏感为主,不同影响因子在敏感性分区的变化范围不同,其中地形因子和植被覆盖与管理因子对土壤侵蚀最为敏感。 相似文献
56.
The light demands of seaweeds is an interesting and rather complex phenomenon because they depend not only on the species
but also on their different development stages. Even different parts of the same plant sometimes have different light demands.
Light control is an important procedure at large scaleLaminaria nursery stations in China. Technicians and scientists have different viewpoints on the best method to regulate light. A culture
study onLaminaria japonica starting from zoospores to several centimeter sporophytes to find the optimal and critical irradiance ranges for juvenileLaminaria at different development stages added more knowledge on this aspect. Experiment results show gametophytes can not tolerate
irradiance of more than 150 μE m−2s−1 while sporophytes can tolerate more than 519 μE m−2s−1. This big difference starts from the very early stage of 1-to 2-celled sporophytes. The biological basis and mechanism of
this phenomenon need further research.
Contribution No. 1515 from the Institute of Oceanology, Academia Sinica
Contribution No. 1 from the Experimental Marine Biological Laboratory 相似文献
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用长效肥料提高微生物分解海面油膜试验 总被引:1,自引:0,他引:1
氮和磷是限制海洋油污生物降解的重要因素,采用可被微生物分解的两种蜡的混合物,把含有10:1的氮和磷的无机盐粉末包埋起来,制成亲油性且能与油膜漂浮在一起的长效肥料。在室内进行促进海水表面柴油油膜的生物氧化实验,结果表明:制备的长效肥料有促进油膜中烃类氧化微生物的生长和柴油的生物降解作用,实验9天除油率达到57 4%,对照实验仅24.5%。 相似文献
59.
ApplicationofpurplenonsulphurbacteriumRhodopseudomonassp.inspatrearingofBayScallopArgopectenirradiansirradians¥//Theeffective... 相似文献
60.
黑绸Sparusmacrocephalus(Basilewsky)视网膜中存在视杆、单锥和孪生双锥三种光感受细胞,视杆与视锥的比例较大,为67:1。每一双极细胞接受约5—8个视杆的输入,每一神经节细胞接受约17—25个双极细胞输入,表明神经节细胞有较大的感受野。视网膜细胞这种形态组合有利于提高视网膜对光的敏感性,与黑鲷生存的浅海底层弱光环境相适应。黑鲷的视杆色素经测定为视紫红质VP4851(吸收光谱峰值为485nm),其吸收光谱与黑鲷栖息水层中日光能量分布相对应,也与该水层中的生物光场相适应。黑鲷暗视光谱敏感曲线峰值与视紫红质吸收光谱曲线相一致,均在485nm处。此外,黑鲷光谱敏感曲线存在普氏位移,表明黑鲷具有辩色力。 相似文献