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碳酸盐

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The results show that REEs oxide have little effect on the decomposition of carbonate and they improve the sinterability of the raw meal;they also promote the formation of alite and growth of clinker minerals,and have beneficial effect on the uniformity of crystal size and well-distributed minerals. But some REEs result in the corrosion of alite when they are excessive,which may influence the hydration reactivity of alite.When clinker is well sintered, REEs oxide and its tailing improve the strength of cement clinker, and have little effect on setting time of cement.

研究结果表明,稀土氧化物对碳酸盐的分解影响不大,对生料的易烧性有改善作用;稀土氧化物能促进熟料中A矿的形成和矿物的发育,有利于熟料中矿物结晶尺寸和分布均匀,但部分稀土在掺量过量时可能造成矿物的熔蚀,影响矿物的水化活性;在煅烧良好的条件下,稀土氧化物和尾矿对熟料强度有增进作用,对水泥凝结时间影响较小。

The compactness and association of large lucinid bivalves in massive cold-seep carbonates further indicate pronounced, long-lasting seepage of methane occurred antecedently the development of Takangshan Reef.

至於大岗山地区所见岩理致密并且含有许多大型满月蛤贝类的块状冷泉碳酸盐岩,则显示在大岗山珊瑚礁发育之前泥岩基底曾有持续相当长时间甲烷逸出的冷泉作用。

The first, gold exporlation in Northwestwen Guangxi must focus at some areas, where in turbidite strata of Baifeng Formation of Middle Triassic Series and in the upfaulted blocks of the bent locations of deep and great and arcual faults by boundary of underwater carbon platforms.

桂西北地区的金矿床就主要在碳酸盐台地边缘弧形深大断裂的外弧转折部位上盘中三叠统百蓬组地层中寻找。对比金牙金矿,这种位置既是盆地有机流体的集中储集点,又有后期热改造的通道,最有利于金的成矿。

Karstification is the main forming mechanism of the carbonate karst reservoir near the unconformity, and the depth influenced by atmogenic freshwater is about 150 m under the Caledonian unconformity.

岩溶作用是潜山不整合面附近碳酸盐岩岩溶储层的主要形成机理,主要集中在加里东不整合面之下150m的深度范围。

A quantitative correlation between carbon and oxygen isotopes of authigenic carbonates from lake sediments can easily be derived.

用统计方法可以较直接地获得气候要素与湖泊自生碳酸盐碳、氧同位素的定量关系,避开考虑复杂的湖泊物理化学过程,为定量恢复古气候提供了一条便捷途径。

The curve of palaeotemperature is reconstructed on the base of authigenic carbonates oxygen isotope.

1,利用自生碳酸盐氧同位素重建了安固里淖湖区古温度曲线。8507aB.P。

Authigenic carbonates in Jiulong Methane Reef occur in the form of crusts and chimneys.

研究表明,所研究的5块&九龙甲烷礁&地区的碳酸盐岩形态主要以结壳、烟囱等形式出现,结壳的裂隙或孔洞中常常充填有淡黄-白色的文石晶体。

On basis of measurement of homogeneous temperature of inclusions, analysis and calculation of δ〓C and δ〓O, and SEPM analysis, the author has studied the forming temperature of authigenic quartz and carbonate minerals for the first time. Furthermore, the author points out that it is unreasonable to recover paleo-geothermal gradient directly using homogeneous and modern burial depth.

作者在包裹体均一温度测量、碳氧同位素测量和计算及电子探针分析的基础上,首次对吐哈盆地侏罗系自生石英和碳酸盐矿物的形成温度进行了研究,确定了这两种成岩矿物的形成温度,并指出直接用包体均一温度和地层现埋深恢复古地温梯度存在不合理性。

Carbonate cements are the most abundant authigenic minerals in the Palaeogene sandstones of Lishui sag, East China Sea basin .

碳酸盐胶结物是东海盆地丽水凹陷古近系储层砂岩中最为重要的自生矿物,主要类型为铁白云石和方解石。

When palaeoclimate became arid, the content of authigenic carbonate increased, and the proportion of aeolian silty sand in terrigenous clast increased distinctly too.

在高频旋回中,当气候偏干旱时,页岩中的自生碳酸盐含量增加,同时风成粉砂在陆源碎屑中所占的比例也明显升高。

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