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In the Early Ordovician Majiagou Formation, on the east side of the basin, the authors have discovered such potash salts as sylvite, carnallite and rinneite, which is the first discovery of potash salts in the Ordovician in the world.

陕北奥陶系是一个大型海相蒸发岩盆地,笔者在盆地东侧下奥陶统马家沟组,发现了钾石盐、光卤石等钾盐矿物,这是世界上首次在奥陶系发现钾盐。

The structure of prehnite consists of ions Ca~(2+),Al~(3+),OH~- and[Si_3AlO_(10)]_n~(5n-).

葡萄石结构系由 Ca~(2+),Al~(3+),OH~-和[Si_3AlO_(10)]_~5(?-等离子组成,其中层型硅氧骨干系与(001)面平行,相隣的骨干通过离子 Al~(3+)得以结合。

This paper reports the results of highly precise zircon SHRIMP U-Pb dating of quartz albitite in the volcanic-sedimentary series of the Tuolugou cobalt deposit, Golmud, Qinghai. Analyses of eight spots presented 206Pb/238U ages of 455 to 483Ma with a weighted mean age of 468±9Ma, which represents the timing of submarine volcanic exhalation in this area. Therefore, the age of the host rocks of the Tuolugou ore district is redefined as Ordovician, which implies that regionally the main part of the Naij Tal Group should be Early Paleozoic in age.

青海格尔木驼路沟矿区赋矿火山-沉积岩系中的石英钠长石岩样品锆石SHRIMP U-Pb精细测年结果表明,该岩石具有一组8个测点构成的455~483Ma的206Pb/238U年龄数据,加权平均年龄为468Ma±9Ma,应代表本区海底火山喷流作用的时间,因此重新厘定了矿区内含矿岩系的时代为奥陶纪,同时,这一年龄指示区域上纳赤台群主体的时代应为早古生代。

Express as a result that the study area gets close to hydrocarbon generation center, have high-quality coal measures hydrocarbon source rock along with big hydrocarbon generation intensity, so it has abundant gas source and the material foundation to form large scale natural gas reservoir; Evaporitic tidal flat facies of the Ordovician Majiagou Formation in this area is situated in the austral expanded range of the karstification zone, and is the optimum natural gas prospecting targets of the lower-Paleozoic; In the south of study area, there are well-developed delta deposition system sand bodies of Shanxi Formation and Xiashijezi Formation, hence this area becoming the most beneficial Neopaleozoic natural gas enriched region; In this area, the Paleozoic develop various concealed non-structured traps, the natural gas migration and accumulation process is very beneficial and both the cover and the conservancy condition are also very good.

结果表明:研究区紧邻上古生界生烃中心,发育优质煤系烃源岩,生烃潜力大,气源充足,具备形成大型天然气藏的物质基础;区内奥陶系马家沟组发育有蒸发潮坪相沉积,位于北部古潜台的向南延伸带上,是下古生界天然气的有利勘探目标;南部山西组和下石盒子组发育三角洲沉积体系砂体,是有利的上古生界天然气富集区;研究区古生界发育各种隐蔽性非构造型圈闭,天然气运聚成藏过程非常有利,封盖和保存条件也很好。

From the research of the kerogen carbon isotopes of the coal-measure strata in some basins of China (the Carbo-Permian in the Ordos basin, the Triassic in the Sichuan basin, the Jurassic in the Jungar basin and Turpan-Hami basin, the Tertiary in the Yingqong basin) it can be indicated that the Type Ⅲ kerogen has a wide δ〓C range from -21. 2‰ to -27. 6‰, averaging -25‰, which is more enriched in 〓C than sapropel and mixed kerogens.

对我国一些含煤盆地(陕甘宁石碳-二叠、四川三叠系、准噶尔侏罗系、吐哈侏罗系、莺琼盆地第三系)的煤系地层干酪根碳同位素研究表明,煤系地层的干酪根碳同位素组成δ〓C值分布范围为-21.2~-27.6‰,说明其变化范围较宽,平均值为-25‰左右,相对腐泥型干酪根和混合型干酪根较明显地富重碳同位素。

Zirconolite rich ceramics and Perovskite rich ceramics are fabricated for the incorporation of simulated trivalent actinide wastes, and the physical properties、XRD、SEM and durability tests are performed.

针对模拟三价锕系元素的固化,分别合成了富钙钛锆石固化体和富钙钛矿固化体,并对其主要性能进行了分析和比较,为其对三价锕系元素的固化提供了依

The multiphase tectonic activities above clearly controlled the move and gather of salifying brine, the strongth of salt-forming and the deposition of salt-bearing strata. With the pass of time, the salt-bearing strata thickened gradually from northwest to east and southeast, and the distribution of the thickness trended towards complicated; the measurement of the halite deposition extended towards east too; in the early Palaeogene and the Neogene, strong multiphase tectonic activity was a disadvantage to salt-forming, but in the middle and late Palaeogene, weak multiphase tectonic activity, which resulted in slow and sustained subsidence of the basin, was greatly advantaged to it, especially to potash-forming.

古近纪和新近纪成盐卤水的迁移和聚集、成盐作用的强弱以及整个含盐系的沉积发育明显受到上述构造活动的控制:含盐系的厚度随时间由北西向东、向南逐渐增厚,且厚度分布逐渐趋于复杂化;石盐岩的沉积规模和范围也逐渐向东扩大;古近纪早期和新近纪强烈的构造活动对于成盐作用而言是一种干扰因素,而古近纪中、晚期相对较弱、导致盆地缓慢持续沉降的构造活动对成盐,尤其对成钾作用则极为有利。

Kowloon also known as jade, jade Huaan, origin JIANGBEI Creek in Kowloon, the number of the most abundant reserves°ancient call this stone as plum stone, marble, stones are one of China's top ten, and its scientific name banded calcium silicon qualitative angle rocks, sedimentary rocks by heat changes in the role of self-formation, since their deposition age between about§°°òêto§°òê.

九龙璧玉也称华安玉,产地在九龙江北溪,储量最丰富的数华安县,古代称此石为梅花石、云石,是我国十大奇石之一,其学名为条带状钙硅质角岩,系由沉积岩热力自变化作用形成,其沉积年代距今约二亿四千八百万年至二亿四千三百万年之间。

Cold places like cold stone substrate, transparency, quality nourish, low hardness, gloss strong line better varieties; soft ground nearly frozen to substrate, but the lack of transparency; just manner, then the hardness high, often with quartz quality of sand screw; hard the worst quality, hardness, opacity, gloss weak, often more impurities, and rock in the gravel. 3, defects, including impurities and cracks in the stone.

冻地的底质似冻石、透明度高、质细润、硬度低、光泽强,系较佳品种;软地的底质接近冻地,但透明度不足;刚地,则硬度偏高,常含石英质砂钉;硬地的品质最差、硬度大、不透明、光泽弱,常有较多杂质和围岩中的砂砾。3、瑕疵,包括石中的杂质和裂纹。

Paleozoic stratum can be separated east and west stratigraphical areas, according to lithological character and palaeontological information, contacted relationships and diversification of stratigraphical units in horizontal and vertical etc. The stratums in west area can be divided Devonian-Carboniferous Nanduan formation and Permian Laba formation, which is passive continental margin-bathyal depositional sequences comprised argillaceous and detrital rocks, small siliceous and carbonatite in upper. The stratums in east area can be divided lower-middle Devonian Wenquan formation and middle-upper Devonian Manxin formation, upper Devonian-lower Carboniferous Pingzhang formation, Carboniferous-Permian Yutangzhai formation, middle Permian Damingshan formation, upper Permian Shifodong formation respectively, moreover, middle-upper Permian Huoju formation is exposed in Menglian area.

根据地层的岩石组合、古生物、接触关系和地层单位的纵横向变化等特征,晚古生代的地层明显的可分为东、西两个地层小区:东部地层小区从下至上可划为泥盆—石炭系南段组、二叠系拉巴组,为一套泥质岩、碎屑岩,上部夹硅质岩、碳酸盐岩建造,属被动大陆边缘斜坡—半深海沉积;西部地层小区由下至上划分为下—中泥盆统温泉组、中—上泥盆统曼信组、上泥盆—下石炭统平掌组、石炭—二叠系鱼塘寨组、中二叠统大名山组、上二叠统石佛洞组,此外,在孟连一带尚出露中—上二叠统火居组。

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