syngenetic 中文意思是什麼

syngenetic 解釋
共成的
  1. There are typical laminated structure, soft sedimentary - slipping deformed structure, syngenetic brecciated structure in the ore which are the mirror of syngenetic sedimentation. the other type of ore has the charactristic of epigenetic mineralization, which is called as telescoped ore. the ore occurs in vein, pocket, lensoid and bedd

    礦石中發育典型的紋層狀構造、軟沉積滑動變形構造、同生角礫構造等反映同生沉積特徵的礦石構造；另一類礦石具有明顯的後生成礦特點，稱之為疊生改造型礦石，礦石產于脈狀、囊狀、透鏡狀及似層狀礦體中，與燕山期巖漿巖及斷裂裂隙構造關系密切。
  2. There are a series of lead - zinc polymetallic deposits, such as fozichong, dongtao, xiashui, wenlongjing and jilongding distributed along the fault zone. these deposits have some similiar features : ? ll of them are bounded in the strata of lower palaeozoic group ; ? ain orebodies occur as stratiform or stratoid form with occurrence consistent with that of host strata ; ? tratiform skam or baritic rock are the direct country rock of orebodies ; ? ypical syngenetic sedimentary fabric preserved in the ore. these deposits may be included in the same metallogenic series

    佛子沖、東桃、下水、文龍徑、雞籠頂等一系列鉛鋅多金屬礦床沿該斷裂帶分佈，這些礦床雖然在成礦規模、賦礦層位和礦石礦物組成等方面存在一些差異，但均產于下古生界地層中；主要礦體呈層狀、似層狀產出，與地層產狀大體一致；直接賦礦圍巖為層狀綠色巖或重晶石巖；礦石中保留有典型的同生沉積組構。
  3. In the upper jurassic to tertiary, there is the alkali diagenetic ambient, in which the inter - pore fluid is inherited from the buried syngenetic water, i. e., alkali saline

    上侏羅紀至第三系為堿性成巖環境，隙間流體繼承了封存同生水特徵，為堿性鹽鹵水。
  4. The green - rock has following features : ? he stratiform green - rock ' s mode of occurrence is conformable with that of the strata, and there are typical syngenetic sedimentary structure in the rock ; ( 2 ) the stratiform green - rock is constituted mainly by bistagite without zonal distribution around magmatic rocks

    作者首次提出賦礦的綠色巖建造概念。其中層狀綠色巖是佛子沖礦田層狀、似層狀礦體的直接賦礦圍巖，這種層狀綠色巖一直被視為矽卡巖。
  5. Two kinds of ore have been identified. the first type is characterized by syngenetic sedimentation, which is called as hot - water sedimentary ore. the ore emerges in bedded orebodies which have stable thickness

    作為典型礦例的佛子沖礦田主要產于下志留統細碎屑巖夾碳酸鹽巖地層中，作者首次在礦田內發現了兩種不同礦石類型：一類礦石具有典型的同生沉積特徵，稱之為熱水沉積型礦石，礦石產于層狀、似層狀礦體中。
  6. By analyzing and generalizing minerogenetic and geological background, mineral constituent, rare - earth element, isotope and typomorphic feature of sulpurization mineral, finally, we made a conclusion that fankou desposit resulted from the hot spring eruption at the bottom of sea, it has a character of syngenetic sedimentary deposit, which was affected by the late hydrothermal superimposed and light rebuilding after it came into being, which is typical sedex bedded - controlled deposit

    通過對凡口礦床的成礦地質背景、礦物成分、稀土元素、同位素以及的黃鐵礦、閃鋅礦、方鉛礦標型特徵進行了分析總結，確定了凡口礦床是海底熱泉噴溢形成的，同時又受到後期熱液輕微疊加改造，屬于典型的sedex型層控礦床。
  7. Relocation of syngenetic uranium may explain a characteristic feature of the deposits.

    同生鈾的重新分佈可以用來解釋礦床的一個典型特徵。
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