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151.
本文针对硬地层钻头寿命短、钻进效率低等问题,研制了一种新型超高胎体偏心齿钻头。该钻头通过条状或类条状设计提高了单齿工作压力;偏心布齿设计改善了钻进过程中钻头的切削齿受力状态,不但提高了钻头的强度,而且使得排浆更加通畅;扭面后支撑结构保证了钻头具有最高可至30 mm的超高胎体工作层。在钻头的制造工艺上,将无压烧结、热压烧结与二次镶焊3种工艺进行了有机结合,钻头金刚石热损伤小、钻头胎体强度高,保径优势明显,为深部硬地层高效长寿命钻进提供了技术支撑。 相似文献
152.
超硬材料在工业发展中扮演着举足轻重的角色,特别是地质钻探行业中超硬材料的研制与应用更显突出。以前钻探界有句话:“有什么样的磨料就有什么样的钻进设备和钻进工艺”,这充分说明了它们的因果关系。金刚石钻头随着人造金刚石的品种、结构、性能、品质等方面不断提高,很大程度上满足了地质钻探行业的需求,并推动了钻探行业的飞速发展;同样钻探应用中提出的新需求,又不断促进超硬行业继续探索。两者相辅相成,互相促进,共同发展。本文结合大量实例阐述了地质钻探行业中使用的超硬产品的特点、种类、性能等。真切地期待未来超硬材料能够更精更新,更多地在钻探产业实现创新突破。 相似文献
153.
154.
通过绳索取心钻进金刚石钻头选型试验,介绍了广西资源县向阳坪铀矿区“打滑”地层中绳索取心钻进存在的问题及采取的技术措施。 相似文献
155.
The Neoproterozoic Aries kimberlite was emplaced in the centralKimberley Basin, Western Australia, as a NNNE-trendingseries of three diatremes infilled by lithic-rich kimberlitebreccias. The breccias are intruded by hypabyssal macrocrysticphlogopite kimberlite dykes that exhibit differentiation toa minor, high-NaSi, olivinephlogopiterichteritekimberlite, and late-stage macrocrystic serpentinediopsideultramafic dykes. Mineralogical and geochemical evidence suggeststhat the high-NaSi, olivinephlogopiterichteritekimberlite was derived from the macrocrystic phlogopite kimberliteas a residual liquid following extended phlogopite crystallizationand the assimilation of country rock sandstone, and that themacrocrystic serpentinediopside ultramafic dykes formedas mafic cumulates from a macrocrystic phlogopite kimberlite.Chemical zonation of phlogopitebiotite phenocrysts indicatesa complex magmatic history for the Aries kimberlite, with theearly inheritance of a range of high-Ti phlogopitebiotitexenocrysts from metasomatized mantle lithologies, followed bythe crystallization of a population of high-Cr phlogopite phenocrystswithin the spinel facies lithospheric mantle. A further oneto two phlogopitebiotite overgrowth rims of distinctcomposition formed on the phlogopite phenocrysts at higher levelsduring ascent to the surface. Ultra-violet laser 40Ar/39Ar datingof mica grain rims yielded a kimberlite eruption age of 815·4± 4·3 Ma (95% confidence). 40Ar/39Ar laser profilingof one high-Ti phlogopite-biotite macrocryst revealed a radiogenic40Ar diffusive loss profile, from which a kimberlite magma ascentduration from the spinel facies lithospheric mantle was estimated(assuming an average kimberlite magma temperature of 1000°C),yielding a value of 0·232·32 days for thenorth extension lobe of the Aries kimberlite. KEY WORDS: 40Ar/39Ar; diamond; kimberlite; mantle metasomatism; phlogopitebiotite 相似文献
156.
157.
2009年中国已成为世界第二大钻石消费国,在国内市场上能见到各类颜色或净度经过处理的钻石及合成钻石。以国检中心(NGTC)近年来在钻石鉴定方面的部分成果为基础,综合论述了国际上钻石鉴定与研究的进展,并介绍了国内、外珠宝实验室鉴定多过程处理钻石的指标。 相似文献
158.
L. F. DOBRZHINETSKAYA R.WIRTH D. RHEDE Z. LIU H. W. GREEN 《Journal of Metamorphic Geology》2009,27(9):607-620
Exsolution lamellae of pyroxene in garnet (grt), coesite in titanite and omphacite from UHPM terranes are widely accepted as products of decompression. However, interpretation of oriented lamellae of phyllosilicates, framework silicates and oxides as a product of decompression of pyroxene is very often under debate. Results are presented here of FIB‐TEM, FEG‐EMP and synchrotron‐assisted infrared (IR) spectroscopy studies of phlogopite (Phlog) and phlogopite + quartz (Qtz) lamellae in diamond‐bearing clinopyroxene (Cpx) from ultra‐high pressure (UHP) marble. These techniques allowed collection of three‐dimensional information from the grain boundaries of both the single (phlogopite), two‐phase lamellae (phlogopite + quartz), and fluid inclusions inside of diamond included in K‐rich Cpx and understanding their relationships and mechanisms of formation. The Cpx grains contain in their cores lamellae‐I, which are represented by topotactically oriented extremely thin lamellae of phlogopite (that generally are two units cell wide but locally can be seen to be somewhat broader) and microdiamond. The core composition is: (Ca0.94K0.04Na0.02) (Al0.06Fe0.08Mg0.88) (Si1.98Al0.02)O6.00. Fluid inclusions rich in K and Si are recognized in the core of the Cpx, having no visible connections to the lamellae‐I. Lamellar‐II inclusions consist of micron‐size single laths of phlogopite and lens‐like quartz or slightly elongated phlogopite + quartz intergrowths; all are situated in the rim zone of the Cpx. The composition of the rim is (Ca0.95Fe0.03Na0.02) (Al0.05Fe0.05Mg0.90)Si2O6, and the rim contains more Ca, Mg then the core, with no K there. Such chemical tests support our microstructural observations and conclusion that the phlogopite lamellae‐I are exsolved from the K‐rich Cpx‐precursor during decompression. It is assumed that Cpx‐precursor was also enriched in H2O, because diamond included in the core of this Cpx contains fluid inclusions. The synchrotron IR spectra of such diamond record the presence of OH? stretching and H2O bending motion regions. Lamellar‐II inclusions are interpreted as forming partly because of modification of the lamellae‐I in the presence of fluid enriched in K, Fe and Si during deformation of the host diopside; the latter is probably related to the shallower stage of exhumation of the UHP marble. This study emphasizes that in each case to understand the mechanism of lamellar inclusion formation more detailed studies are needed combining both compositional, structural and three‐dimensional textural features of lamellar inclusions and their host. 相似文献
159.
西藏罗布莎蛇绿岩铬铁矿中金刚石的研究 总被引:27,自引:3,他引:27
在西藏罗布莎豆荚状铬铁矿中发现过金刚石,但迄今仍有人因为自己所取的小试样中没有分离出金刚石而否定罗布莎等地金刚石的存在。由于金刚石涉及西藏雅鲁藏布江缝合线和蛇绿岩、铬铁矿成因等问题,笔者重新在罗布莎铬铁矿中取样,经过选矿,又在1500kg样品中选出了25粒金刚石和近70种伴生矿物。这就表明西藏金刚石是的确存在的,而且它和蛇绿岩的铬铁矿同是深部成因的产物。 相似文献
160.
湖南金刚石内部不均一性特征研究 总被引:1,自引:0,他引:1
将湖南金刚石加工成片,利用宝石显微镜,偏光镜,阴极发光(CL)仪和傅里叶红外光谱(FTIR)仪对其内部显微特征进行了研究,发现金刚石的颜色深浅不一,内外颜色差异明显,呈带状,斑状分布;金刚石由生长中心至边缘,氮含量也有较大变化,中心与边缘最大相差约50倍,氮的富集类型由中心向边缘表现出B中心所占的比例越来越小,金刚石的类型也相应从I型→II型或I-aAB型→-I-aA型等,这些不均一性特征,反映金刚石在生长过程中环境条件发生了变化,以及生长期后可能受到了改造。 相似文献