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岩床

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L the normal zonning in order of greisen type tin deposit 〓tourmalite type tin deposit 〓 cassiterite quartz type tin deposit 〓cassiterite sulfide tin deposit copper-lead-zinc 〓 sulfide deposit 〓lead-zinc sulfide deposit 〓antimony deposit, which may be related to the high-level em placement of the intrusions;2 the reversed zoning in order of lead-zinc deposit 〓copper-lead-zinc deposit 〓tin polymetallic deposit, which may be result from the descending of heat centre of the intrusions with their cold and solidification.

该成矿系列的矿床在空间上有序分带,即以岩体为中心的顺向分带为:云英岩型锡矿床〓电英岩型锡矿床〓锡石石英型锡矿床〓锡石硫化物型锡矿床〓铜铅锌金属硫化物矿床〓铅锌硫化物矿床〓锑矿床,逆向分带为:锡多金属矿床〓铜铅锌硫化物矿床〓铅锌硫化物矿床,造成这种分带现象的内在因素是高热能且富含矿热液的黑云母花岗岩的高侵定位和岩体热中心的向下移动。

This study was only focused on the No.Ⅰore body. Based on detailed logging and dating results, it is considered that mineralization of the Cu_Au porphyry occurred in Late Jurassic. The formation of the ore body is related to the Late Jurassic augen quartz phenocryst_bearing hornblende_quartz diorite porphyrite intrusion(J3δομ).

通过对雄村铜金矿床Ⅰ号矿体详细的地质编录和测年成果,发现雄村斑岩型铜矿床形成于晚侏罗世,矿体的形成与晚侏罗世侵位的、含眼球状石英斑晶的闪长玢岩(J3δομ)有关,成矿岩体呈不规则的岩枝状,全岩矿化,岩体中Au的平均品位大于1g/t,Cu含量大于0.7 %。

Students look at the back, chichi pour in rock bed, not a day to eat, drink, and say a word.

看着同学远去的背影,琪琪一下子倒在岩床上,一天都没有吃东西、喝水、说一句话。

Results The superior wall of cavernous sinus, longitudinal trapezoid in shape, was limited laterally by anterior petroclinoid ligament and lateral margin of anterior clinoid process, and medially by the dura of the diaphragma sellae, anteriorly by the base of anterior clinoid process and the falciform dural fold, and posteriorly by the posterior petroclinoid ligament.

结果 海绵窦上壁呈纵长的四边形。外侧界为前床岩韧带和前床突外缘;内侧界为鞍隔的硬膜缘;前界为前床突基底部和镰状硬膜皱褶;后界为后床岩韧带。

There are three genetic types of mineral deposits in the Beiya ore district:① Cu-Au polymetallic deposits related to alkaline porphyries, comprising porphyritic Cu-Au deposits and polymetallic skarn deposits related to quartz-albite porphyry and quartz-K-feldspar porphyry;② Fe-Au deposits related to gabbro or basalt magma, consisting of magmatic Fe-Au deposits and sedimentary polymetallic deposits formed in caves and lakes; and ③ palaeo-placers formed at the weathering surface, in lakes and in karsts.

北衙金矿有3种成因不同的矿床:①与碱性斑岩有关的铜金多金属矿,包括与石英钠长斑岩和石英正长斑岩有关的斑岩型铜金矿床和矽卡岩型多金属矿床;②与辉长-玄武岩浆有关的铁金矿床,包括熔浆型铁金矿床和喷流沉积型多金属矿床,后者又有洞穴和湖相沉积环境之分;及③古砂矿,有古风化壳型砂矿、河湖相古砂矿和洞穴沉积古砂矿。

Late Permian to Triassic rifting and subsidence resulted in the deposition of as much as 9 kilometers of Triassic strata, locally injected with sills.

二叠纪晚期到三叠纪断裂和下沉作用形成了大约9千米厚的第三纪沉积地层,在其中有岩床的切入。

Then came the Burning Legion and the Great Sundering, which shook ancient Kalimdor to the bedrock.

然而,燃烧军团的来临和世界大分裂震荡了整个原始卡利姆的岩床

Soil near the surface and eventually reached bedrock, the hardened lava of the Columbia Plateau.

洪水冲洗掉地表附近松软的风化土,最终到达了岩床,哥伦比亚高原上坚硬的火山岩。

The waters scoured off the soft, windblown soil near the surface and eventually reached bedrock, the hardened lava of the Columbia Plateau.

洪水冲洗掉地表附近松软的风化土,最终到达了岩床,哥伦比亚高原上坚硬的火山岩。

They not only occur in deep ocean basins such as in the central North Atlantic where they were deposited below CCD, but they extend up the continental slopes and rises, such as in the Alps, including the Gampu area , in the Carpathian Mountains (Austria, Slovakia, Poland, Romania), in Spain, in Turkey and in the Exmouth Plateau (Legs 122 and 123) in northwest Australia.The Upper Cretaceous reddish marlstones in Italy are particularly similar to the Upper Cretaceous Chuangde formation red beds in the Tibetan Himalayas. In summary, the Upper Cretaceous redbeds have several characteristic as follow:(1) very low TOC, only 0~0.3%;(2) wide distribution throughout the Neo-Tethys, from north Atlantic to the west, to Exmouth Plateau to the east;(3) Sedimentary environment of the red beds varied from oceanic basin, to slope/rise, to outer shelf. Most comment is pelagic and hemipelagic.

床得组泥灰岩〓含量0.26~5.62%,远远高于奥地利和意大利红层0.45~0.82%,并出现金属元素高含量,平均达926ppm,以高含量Ba、Cu、Zn、Cr、Ni、Th等元素为特征;2)床得组红层〓相对于定日地区同期海相碳酸盐〓整体负向偏移量达2.0‰,而在其床得组红层内部〓自下而上一直攀升,自-1.5‰~0.0‰之间上升到0.0‰~1.0‰之间;定日贡扎剖面相当于江孜床得组红层的Santonian-Campanian期,〓也出现一弱负向偏移,偏移量达-0.8‰;3)红层内锶同位素〓比值为最低值,同期定日地区也出现锶同位素低值;4)床得组部分层段的泥晶灰岩出现丰富的有孔虫,其中尤以浮游有孔虫最为繁盛,与江孜地区临近的浅海陆棚相的定日—岗巴地区此时期出现自Cenomanian-Turonian界线生物绝灭后的生物辐射期。

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