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1.
笔者于1989年夏指导学生野外实习过程中,在桂东南某杂岩体中发现了一种含月光石的基性岩。该岩石产于某杂岩体的基性岩体中、基性岩体出露呈弯月状,面积约0.2km~2。经初步鉴定,含月光石基性岩具辉长辉绿结构,主要由含钛辉石、拉长石及少量橄榄石、月光石、钾长石、磁铁矿等组成,暂定名为“含月光石辉长岩”(或星光墨玉)。该岩石结构致密坚硬,经加工磨光性能良好,抛光面青黑油亮,在青  相似文献   

2.
本文运用热力学计算公式对大连马桥子辉长辉绿岩结晶温度进行了尝试性的推算。计算结果表明辉长辉绿岩岩体温度下降缓慢,与围岩长时间作用,则形成了石棉矿床。  相似文献   

3.
广西芒场隐伏岩体通过系统研究,其外部形态凹凸不平,呈现以北西向为主和北东两向展布的串珠状凸起;岩体划为A、B、C三次侵入,A次为中性玢岩属正常类型的次钙碱性岩,B、C次花岗岩属铝过饱和的钙碱性-钙性岩;C次花岗岩顶部具有似伟晶岩壳,可作为两次花岗岩先后侵位的重要标志;B次钾长石属中正长石系列,C次钾长石属低正长石-最大微斜长石系列,B、C次斜长石均属高钠斜长石;黑云母多为含锂铁叶云母;黑云母和长石是成矿物质的重要载体矿物;岩体成因类型属燕山晚期的壳源重熔岩浆型花岗岩(与大厂花岗岩同源)即S型花岗岩,岩体就位深度约为2.5-3km,属浅成相:隐伏花岗岩体是一典型的富含钨锡等多金属岩体,与本矿田锡多金属矿床的形成有密切的成矿关系。  相似文献   

4.
Kalarsky岩体是沿阿尔丹南部边缘分布的规模巨大的DjugdjurKalarsky辉长-斜长岩岩带的一部分。本文研究了代表典型地球早期(前寒武纪)发展史、在行星水准上发育的这个特殊杂岩体的构造-物质组分、形成的阶段性及其继后构造演化。辉长-斜长岩杂岩体产于前寒武纪克拉通化地块交接处及其褶皱的流动性较高的框架中。该杂岩体由两个岩浆岩共生组合组成:硅铝质(斜长岩及辉长-斜长岩)及镁铁质(基性-超基性岩)。体积上前者明显小于后者。这两个岩石共生组合的锶同位素比值都特别低,说明其原始岩浆的地幔属性,是在一个相对宁静的背景中在早期分异出来的产物。辉长-斜长岩杂岩体的演化明显分3个阶段:早期是圈闭结晶岩并将其极度加热的阶段,是庞大的具对称构造的地块的形成阶段;中期是地块的最终固结阶段,在此期间发生了褶皱变形,是高压变质作用的初期阶段;晚期是发生刚性变形,形成辉长-斜长杂岩岩体的岩浆岩岩墙群、链状构造及雁行构造,并发生最大高压变质作用的阶段。文中对与辉长-斜长岩杂岩体共生的似榴辉岩也进行了探讨。  相似文献   

5.
通过地质填图和钻探工程控制,大致查明了盂县潘家会矿区辉长苏长岩体的分布范围、规模、形态、产状以及岩体的含矿层位等,并通过区内成矿地质背景和矿床特征的分析,充分说明了该区辉长苏长岩体成矿地质条件较好,可望提交一个与基性岩有关的多金属矿床找矿基地。  相似文献   

6.
本文介绍了济南北部中基性杂岩体中首次发现的黑榴霓辉正长伟晶岩和黑榴霓辉霞石正长伟晶岩的岩石学特征,并对其成因作了探讨。  相似文献   

7.
应用元素地球化学方法.研究了勉略带中辉长辉绿岩的相关特征.结果表明.勉略蛇绿构造混杂带内的辉长岩属高铝强碱质辉长岩类,是地幔橄榄岩部分熔融的产物。辉绿岩墙群属强碱铝质基性岩类,过渡族元素蛛网图与辉长岩类几乎完全相同,其不相容元素与辉长岩类总体趋势相一致.反映了一种递进岩浆演化趋势。因此,本区辉长岩与辉绿岩墙群具同源岩浆分异演化的地球化学特征.其均为勉略蛇绿岩的重要组成端元。  相似文献   

8.
通过35 km21/10000的地质填图和1/5000的地面磁法及部分地区的激电、视电阻率和岩体出露地段的化探工作,对辉长苏长岩体的赋存状况和成矿远景提供了第一手资料.根据地质和物化探理论与外地实验经验,本区辉长苏长岩体有利于形成钒钛磁铁矿床,对铜、镍、钴等硫化矿的赋存条件也具有良好的标志.  相似文献   

9.
辉绿岩是一种基性浅成侵入岩,有人把具辉绿结构的基性熔岩或次火山岩也称为辉绿岩。辉绿岩结构致密、质地细腻、耐磨、耐酸、耐腐蚀,不仅是铸石的原料,而且是优质建筑材料,广泛用于建筑物的室内外装饰。近年浙江神舟石材有限公司和武义神舟宝石工艺品厂将武  相似文献   

10.
广西岑溪地区长岗顶花岗岩体是一个同源岩浆4次侵入而成的复式岩体,由4个大致呈环状分布的龙登岩体、陂头冲岩体、旧村岩体和新里岩体组成.复式岩体内部发育叶理构造,其产状与岩体接触面产状一致,是岩体就位过程中形成的原生构造.研究表明,长岗顶复式岩体就位机制是典型气球膨胀就位模式.侵入就位顺序依次是龙登岩体→陂头冲岩体→旧村岩体→新里岩体.  相似文献   

11.
1 INTRODUCTION The first published records of genus Batra-chospermum Roth in China are from Jao (1941), when eleven taxa were reported. Since then, Shi, Hu and Kumano (1993), Shi (1994a, 1994b), Hua and Shi (1996), Xie et al. (1999, 2003), Xie and Shi (2003) have described in more detail the species from China. To date, 23 taxa of Batrachospermum Roth in China have been reported, of which, B. yunnanense, B. nothocladoideum and B. transito-rium are new species of this genus, and are…  相似文献   

12.
The effects of recombinant eel growth hormone (reGH).methyltestosterone (MT)and L-thyroxine (T4)on the growth of red sea bream. Pagrosomus major.were investigated.Administration of reGH to fry by immersion at 2 mg 1 for 2 hevery 5 dsys resulted in significant increase in both weight and length.but the condition factor (CF) diminished relative to that of similarly treated controls over the 37day treatment period.Immersion in 0.1 mg:1 T4 also resulted in significant increase in both weight and length and higher survival rate of test fry compared to the controls. Immersion in MT had less effect on growth and high-dose resulted in high mortality.In the second study.injection of 2 μg reGH(gwk)caused a significant increase in the specific growth rate (SGR) of test red sea bream fingerlings relative to that of the controls during the 4-week treatment period and maintained the increasing trend over the post-treatment period (weeks 4-6).Injection of MT at a dosage of 1μg (gwk) resulted in a significant in-creas  相似文献   

13.
Investigations of natural and artificial radioisotopes including 90Sr,137Cs, gross B and U carried out in the Yellow Sea and adjacent southeast area in 1963. 1964, 1975 and 1978 showed that radioactive pollution by 90Sr and 137Cs from atmospheric fallout had gradually decreased with time due to the cessation of atmospheric nuclear weapons tests in the 70s. The distributions of natural and artificial radioactive isotopes (U, Ra, Th. 40K and 137Cs) in sediments southwest of Jizhou Island were uniform. The more uniform may be related to the soluble species of U[Uo2(CO3)4] in the seawater.The high value of Th at stations 3 and 6 was related to the sandy clay sediment; the low value at station 8 was related to sandy sediment. The content of 137Cs in the eddy area being less than about half of that in the China inshore area showed that the source of Cs may be insufficient orthat the conditions for enriching " Cs in the circulation eddy area were not favorable.  相似文献   

14.
吉南候家屯组与辽东小东沟组在辽东北部连成一体,以往地层划分和对比上的分歧,皆由王钰等定义小东沟组含有熔岩——“为小岭期火山喷发初的火山活动产物”所致。小东沟组、候家屯组为独立于辽东小岭组,吉南果松组火山岩之外的地层体,为干旱炎热气候条件下的河湖相沉积。辽东梨树沟组建立时未明确定义,建组剖面仅共分二层,为凝灰岩、凝灰质砂岩夹砂页岩,多数研究者将其理解为小岭期火山喷发的尾声产物,无疑是正确的,但近年已人为地演义为“远火山相和湖相”(沉积),并与辽西九佛堂(沙海)组对比,已失去岩石地层单位组的客观性、物质性及组内岩性、岩相的一致性。现据“组应概分,不易细分”等有关原则,建议废弃梨树沟组名称,将与小岭组有成因联系的远火山相产物(包括夹层)划归小岭组,其上部确与小岭期火山喷发无关的河湖(沼)相沉积归于聂尔库组  相似文献   

15.
Synedra ulna var. repanda Q. X. Wang & Q. M. You, a new variety of Synedra (Bacillariophyta) from Xinjiang, China, is described and illustrated, and the characteristic of the variety: includes undulate-linear valves and straight pseudoraphe, differs from other species of Synedra.  相似文献   

16.
初步研究了细基江蓠繁枝变种(G. tenuistipitata var. liui)和细基江蓠(G. tenuistipitata)切段培养的适宜培养基及其切段的再生特点。在此基础上,还研究了几种植物生长调节剂对江蓠藻体切段再生的影响。研究表明,江蓠藻体在改良PES培养基中生长良好。两种藻体的外皮层细胞均可产生长成新枝的生长点,并且表现出相同的再生极性。无论细基江蓠繁枝变种还是细基江蓠的切段都是在形态学上端切口处产生新枝,下端不再生;带分枝的切段,其分枝断口处亦可再生新枝。适宜的植物生长调节剂可明显促进藻体芽的产生和生长。1 m g/ LBA 明显促进细基江蓠繁枝变种切段的再生,2 m g/ L BA+ 0.5 m g/L NAA 显著促进细基江蓠切段的再生  相似文献   

17.
JCZ─1超宽频带地震计是为中国甚宽频带数字地震观测试验系统研制的新型仪器,由一个垂直向和两个水平向地震计组成,频带为DC─20Hz。每个地震计分别有两个通道输出:20Hz─360秒的速度平坦输出和360秒─DC的加速度平坦输出,复盖了从短周期地震波至固体潮汐的宽广频带。仪器具有高灵敏度、低噪声特点,动态范围大于140dB。地震计采用力平衡式的负反馈系统,传递函数稳定,具有密封、磁屏蔽和高精度恒温功能的环境保护装置,有效地抑制了大气压力、外部磁场及温度变化对仪器的影响,使地震计在超低频端也能稳定工作。  相似文献   

18.
Unialgal explants from Luminaria digitata, and from a variety of red algae were obtained by hand removing the visible epiphytes, and stirring the tissue in the presence of glass beads. Two antibiotic mixtures were found to be efficient in removing the contaminating fungi and bacteria from the algae. The procedure proved suitable as a primary step in the tissue culture of the investigated species.  相似文献   

19.
Three new species of Batrachospermum Roth (Batrachospermales, Rhodophyta) from China are described in this paper. B. yunnanense sp. nov. has long-cylindrical trichogynes with long stalks and is diagnostic of section Virescentia. Within this section, B. yunnanense is similar to B. helminthosum Bory emend. Sheath et al., but it is dioecious and has curved carpogonial branches, while the latter is monoecious and has straight carpogonial branches. It is also similar to B. transtaganum Reis, but it differs from the latter in long carpogonia,big carposporophytes and carposporangia. It is considered that B. nothocladoideum sp. nov. is assigned to section Contorta, subsection Kushiroense, because its carpogonial branches are twisted and gonimoblast filaments are loosely agglomerated. This new species similar to B. iriomotense Kumano, but with short fascicles, long-ovoid or subpyriform cells, numerous terminal hairs, long-ellipsoid trichogynes, big carposporophytes and small carposporangia. The plant is quite tough and cartilaginous and similar to Nothocladus in gross morphology, but its carposporophytes are compact instead of diffuse. This shows that it may be a transitional species between section Contorta and genus Nothocladus. So, B. transitorium sp. nov. should belong to section Contorta, subsection Kushiroense, because of its curved or twisted carpogonial branches and loosely agglomerated gonimoblast filaments, with globose or subglobose cells in fascicles similar to B. spermatiophorum Vis et Sheath, but no colourless spermatiophores. In terms of small and numerous carposporophytes, B. transitorium sp. nov. is similar to some species of section Batrachospermum. However, their other features are unique, indicating its transitional nature between section Contorta and Batrachospermum.  相似文献   

20.
本文根据“七五”项目:《广西贵港市龙头山金矿床地质特征及找矿方向》的研究成果基础上撰写而成。文中侧重地论述了火山机构与矿床特征,并探讨了矿床成困。研究认为:矿床构造是一个晚中生代的残存火山颈机构。在其管道内的隐爆角砾岩、火山角砾岩、角砾熔岩、流纹斑岩和花岗斑岩等岩相带以及中酸性脉岩相,均属贫硅、富钾钙碱性系列的铝过饱和类岩石,是一套陆相中心式火山—次火山喷发—侵入岩系,属同源不同阶段的产物;该矿床金矿体受火山颈机构内的角砾状岩石及其内外接触带的断裂构造控制,多呈直立脉状,具有火山岩型与断裂充填型两类金矿化;成矿物质与流体主要源于火山岩浆喷气、热液,应属火山—次火山岩热液型金矿床。  相似文献   

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