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Here is Belladonna, the Lady of the Rocks

这是贝洛多纳,岩石的女主人

The porosity of sandstone can be 20% or more, which means that a cubic metre of rock say the size of a large fridge, can absorb 200 or more litres of water.

砂岩的孔隙率可能是20%或者更多,这就好比在一个像冰箱大小的一立方米岩石中,能够吸收200或者更多公升的水。

The research shows that in the Yinggehai basin, the formation of CO_(2) reservoir which is crust-sourced and crust-mental-mixed-sourced, mainly controlled by local action of hot fluid in the mud diapir area which is multi terms and multi zones and by physical-chemical mechanism of very thick marine calcareous sandstone and mudstone of Pliocene-Miocene. The volcano- and mantle-sourced CO_(2) in the Qiongdongnan basin and Pearl River Mouth basin is mainly controlled by volcanos activities and by the exist of large faults which reached to base to connect the gas from the mantle. According to different mechanism ang formation of reservoir os the the crustal rock-chemical genesis and volcano-and mantle-sourced CO_(2), we can follow the source of it, analysis and predict the migration and accumulation and distribution model of gas and espacially CO_(2), so as to help to make the plan of petroleum exploration and reduce the risk of exploration.

认为:莺歌海盆地壳源型及壳幔混合型CO2的形成及富集成藏,主要受控于泥底辟热流体晚期分层、分块和多期的局部上侵活动,和巨厚的上新统—中新统海相含钙砂泥岩的物理化学综合作用,且CO2运聚分布规律亦具多期和分层、分区的特点;琼东南盆地东部及珠江口盆地火山幔源成因型CO2则主要受控于幔源型火山活动和沟通深部气源的基底深大断裂的导气配置作用,CO2运聚富集规律与幔源型火山活动及深大断裂的发育展布密切相关,CO2主要来自地壳深部幔源火山活动所伴生的大量CO2;因此,根据壳源岩石化学成因型CO2与火山幔源成因型CO2不同成因机理及成藏条件,可以追踪CO2气源,可分析和预测天然气尤其是CO2的运聚分布规律,可为天然气勘探部署及决策提供依据,可减少和降低勘探风险。

The foliated rock belt is over one hundred meters in width and the intensity of foliation in the center is stronger than that in the margin.

这个片理化岩带有100多来宽,带中央岩石的片理化程度较之于带边缘岩石要强。

Rocky or impermeable sites should be avoided.

多岩石或不易渗透的地区应当避免。

The Shetland Islands, the most northern of the British Isles, are as stark and rugged as they are beautiful.

设得兰群岛位于不列颠群岛的最北部,荒凉而多岩石,非常美丽。

The material for formation of the granitoids isderived from mixing sources of crust and mantle, with decreasing in crust-derived componentsfrom early to late.5. The tectonic setting for formation of the Mesozoic granitoids in the region isdefined as a post-collisional setting. The occurrence of a small part of rocks with characteristics ofcollisional or anorogenic granitoids provides evidence for the continuous process oftransformation of tectonic regime from collisional through post-collisional to anorogenic.6. Themultiple cycles of mantle-derived magma underplating caused by the multiple stages oflithospheric thinning in the Mesozoic result in the partial melting of middle to lower crust orcrust-mantle syntexis to form magmas. The crystallization of these magmas emplacing afterfractionation is responsible for the formation of the Mesozoic granitoids in this region.

形成花岗岩类的成岩物质来自壳幔混源。5、河南省西部地区中生代花岗岩类成岩构造环境为碰撞后环境,部分岩石具有碰撞期或非造山期花岗岩的某些特征,表明碰撞后阶段既是碰撞造山过程的延续,又是向非造山环境的构造转换时期,因而其岩浆活动在一定程度上仍然继承了碰撞前消减时期和碰撞时期已经活化的岩浆源区性质。6、研究表明,区内中生代多阶段的岩石圈减薄作用引发多旋回的幔源岩浆底侵以及中下地壳的部分熔融或壳幔同熔,由此形成的岩浆经分异演化后侵位可以形成区内的中生代花岗岩类。

The thesis also discussed the synthetic influence of above factors on dynamic diagenesis in detail and graded dynamic diagenesis into three types, which were respectively thermally dynamic diagenesis, tectonically dynamic diagenesis and hydrokinetic diagenesis, and then the types of diagenesis controlled by dynamic factors had been studied: 1 thermally dynamic diagenesis, clarified the ration relationship by the conception of the thermally evolving track and the thermally maturity, 2 tectonically dynamic diagenesis, changed the porosity of reservoir mainly by tectonically movement;3 . hydrokinetic diagenesis, changed the physical and chemical properties resist-press intensity of the rock by the participating of liquid.

在研究以上控制因素的基础上,将成岩动力作用分为热动力、构造动力、流体动力成岩作用三种类型:1、热动力成岩作用,运用热演化轨迹和热成熟度的概念研究与成岩作用之间的定量关系,砂岩孔隙度随热成熟度增加而呈指数减小;2、构造动力成岩作用,盆地构造变形可以使砂岩的孔隙体积在相对短的时间内产生明显的变化,构造滑脱推覆作用比水平侧向挤压作用压实减孔量小,可保留更多的孔隙度;3、流体动力成岩作用,化学成岩反应是在流体参与下完成的,它改变了岩石的物理化学性质,改变了岩石的抗压强度。

Its rocks are made of limestone and are formed by water percolating the ground's surface and eroding away everything but the pillars.

石林的岩石由石灰石构成,形成的原因是雨水渗透了地表,腐蚀了一切,只留下诸多岩石柱子。

The base is quite simple, which is ok, but I think it could look a little more nice if the cork 'rocks' were shapes a little more into a more natural looking formation, and given a little more attention with the paintwork as well.

该基地很简单,这是玉,但我认为这可能显得更漂亮,如果软木'岩石'的形状多一点成一个更自然的形成,并给予更多的关注很少与喷漆的。

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