All posts by idbeditor

RS049 Shelly Limestone

Class: 5C Name: Cheuk Wing Yan Year: 2017 – 2018 地質年代: 石灰石沉積在石炭系時期, 在3億年前 化學組成, 鍵及結構: 沒有 (它是化石)         Geological Age: The limestone was deposited in the Carboniferous period, over 300 million years ago Chemical composition, bonding and structure: N/A (It is a fossil)   形成: 風化和侵蝕產生顆粒。被風化的沉積物向下移動。沉積發生。沉積層的重量被堆積和壓實。礦物質會在水中溶解。壓實和膠結疏鬆沉積物會成固體岩石, 形成石灰石。 原生物: 含貝殼石灰岩在淺, 平靜, 溫暖的海洋水域形成。這種類型的環境有碳酸鈣殼可以很容易地從海洋水中提取所需的成分。當貝殼被一層岩石覆蓋時。不斷地積累, 它形成含貝殼石灰岩。                       Formation: Weathering and erosion produce grains. Weather materials are moved downhill by deposition. Sedimentation occurs. Sediment accumulates and compacted…

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RS048 Rhaetic Bone Bed

Class: 5B Name: Tang Chun Tung Year: 2017 – 2018   地質年代:岩石 上三疊統海侵地層的一音分 化學組成, 鍵及結構: 由具有方解石膠結砂質基質的礫岩,和豐富的牙齒,鱗屑以及骨骼所組成 Geological Age: Rock part of a transgressional formation from the Upper Triassic   Chemical composition, bonding and structure: It consists of a conglomerate with a calcite cemented sandy matrix, together with an abundance of teeth, scales and bones 形成:(岩石) 1.風化和侵蝕導致鬆散的碎片和細粒 2.風化物質通過移動或地心吸力而向下移動 3.沉積物和生物的遺骸沉積在湖泊,河流或淺的沿岸海地方 4.沉積物積聚並被上層的重量壓實 5.礦物質溶於水,並將鬆散的泥沙粘合在一起 6.壓實和膠結作用有助於將鬆散的沉積物轉化為稱為沈積岩的固體岩石 Formation:(Rock) (Mineral) 1.       Weathering and erosion produce loose fragments and grains 2.       Weathered materials are moved downhill by moving agents or gravity 3.       Sediment and the…

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RS047 Shelly Limestone

Class: 5B 19 Name: Lo Oi Ying Year: 2017 – 2018 地質年代: 沉積岩中的碳酸鈣濃度,在年代上表現出了明顯的周期性     Geological Age: (Fossil) (Rock) The calcium carbonate concentration in sedimentary rocks shows a clear periodicity in the age   形成: -岩石的風化產物和一些火山噴發物,經過水流的搬運、沉積、形成的岩石 -搬運、沉積的時候 , 有貝殼混在了一起 , 形成的時候, 便有貝殼在岩石裏         Formation:(Rock) -Some weathered product and the product come from Volcanic Eruption, after handling and deposition, it form to become sedimentary rock -when there are after handling and depositing, some shells fix into it, therefore it forms a sedimentary rock…

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RS046 Oolitic Limestone

Class: 5B Name: Leung Hang Yi Year: 2017 – 2018   地質年代:(化石) (岩石) 侏羅紀時期   化學組成, 鍵及結構:(礦物) 方解石 – 碳酸鈣,然後形成小珠狀球體,構造為同心層。 Geological Age: (Fossil) (Rock) Jurassic period   Chemical composition, bonding and structure: (Mineral) Calcite – CaCO3, formed into small pearl-like spheres, constructed as concentric layers. 形成:(岩石) (礦物) 它們主要由隕石組成,這些鮞粒是在溫暖的淺水中形成的砂粒大小的碳酸鈣顆粒,其中碳酸鹽沉積物被水流驅動。   原生物:(化石) 運輸和沈積穀物,動物的骨架或貝殼等主要是非常細的碳酸鹽泥。 Formation:(Rock) (Mineral) They are made up largely of ooids, which are sand-sized, rounded pellets of calcium carbonate formed in warm shallow water where carbonate sediment is moved about by currents.   Living Specimens: (Fossil)…

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RS044 Millstone Grit

Class: 5E Name: WongSunSon Year: 2017 – 2018   地質年代:石炭紀 化學組成, 鍵及結構:磨盤砂組由三十多個單獨命名的砂岩組成,其中一些區域性砂岩,其他地方則較多。其間的泥岩和粉砂岩一般不叫但重要的海洋bandswithin他們命名。 最古老的,囙此最低的演替是蘭開夏厚潘德爾砂礫。這是成功的砂岩稱為布倫南德砂、Warley Wise Grit和格拉辛頓砂礫。這些都是pendleian(E1)的年齡–納繆爾期的最低階段。 Geological Age: Carboniferous age Chemical composition, bonding and structure: The Millstone Grit Group comprises over thirty individually named sandstones, some of regional extent, others more local in their occurrence. The intervening mudstones and siltstones are not generally named though important marine bandswithin them are named. The oldest, and hence lowermost in the succession is the thick Pendle Grit of central Lancashire. It is succeeded by the sandstone known variously as the…

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RS043 Greywacke

Class: 5E Name: Wong Hin Kiu, Andrea Year: 2017 – 2018 地質年代:(化石) (岩石) 古生代 (4.1亿年-2.45亿年前) 化學組成, 鍵及結構:(礦物)       Geological Age: (Fossil) (Rock) Paleozoic Era (541 to 251.902 million years ago) Chemical composition, bonding and structure: (Mineral)   形成:(岩石) (礦物) 雜砂岩一般要先從沉積物(包括礦物和碎石)經過運輸媒介(水)或自然現象(雪崩、地震)而聚集並沉澱,然後再經過強烈的擠壓力而成。 原生物:(化石)         Formation:(Rock) (Mineral) It is commonly formed from sediment deposited (including minerals and rock fragments) to the sea by strong moving agents, such as water or under natural phenomenon, such as avalanches and earthquakes. And they are then compacted…

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RS042 Ganister

Class: 5E Name: Sun Long Yan Year: 2017 – 2018   地質年代:(化石) (岩石) 化學組成, 鍵及結構:(礦物) 由於其需要低磷鐵礦石,他的工藝最初不能由Bessemer’s以外的鋼廠成功使用。化學組成, 鍵及結構是方解石,粘土,粘土礦物,長石,雲母,石英     Geological Age: (Fossil) (Rock) Chemical composition, bonding and structure: (Mineral) An important industrial use of ganister was as the lining bricks for the acid Bessemer converter, a steel-making process developed in 1856.  The Mineral Content are Calcite, Clay, Clay Minerals, Feldspar, Micas, Quartz 形成:(岩石) (礦物) 原生物:(化石) 緻密矽岩是通過土壤形成過程在土壤表層內破壞容易風化的礦物(主要是長石)而形成的。 Formation:(Rock) (Mineral) Living Specimens: (Fossil) Ganisters are formed by the destruction of easily weathered minerals mainly feldspar, within the surface…

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RS040 Flint

Class: 5E (21) Name: Ng Tsz Wing Natalie Year: 2017 – 2018   地質年代:(化石) (岩石) 化學組成, 鍵及結構:沉積岩     Geological Age: (Fossil) (Rock)   Chemical composition, bonding and structure: Sedimentary rock   形成:沉積岩 風化和侵蝕會產生鬆散的碎片和穀物。殘骸和沈積物會沿著河流沉積在湖泊或淺海沿岸水域。 沉積物已經被壓實 由於壓實和膠結作用將鬆散的沉積物轉化為固體岩石稱為沉積岩。             原生物:(化石) Formation: Sedimentary rock   Weathering and erosion produce loose fragment and grains .Sediment and the remains of living organisms are deposited in lakes along rivers or in shallow coastal waters. Sediment have been compacted Because of the compaction and cementation help transform…

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