黃泥帶 的英文怎麼說
中文拼音 [huángnídài]
黃泥帶
英文
yellow ground-
Benthic foraminifer fauna, ams14c dating and acoustic sub - bottom profile was analyzed in the core ey02 - 2 and ey02 - 1 drilled from the muddy deposit in the middle southern yellow sea and the mid - shelf of north east china sea. considering the results of core qc2 ? dz4 and the standard oxygen isotope curves, we discussed the late - quaterenary paleo - environment evolution, benthic foraminifer fauna, paleo - climate, the climate events and water mass in postglacial period, average sedimentation rates, paleo - water depth, origin of sediments, average sea level rise rate in the shelf of south yellow sea and east china sea. at last we discussed the condition of sea level rise in the east china, green house effect and the protection of coastal zone
本文根據南黃海中部泥質區和東海中陸架的兩個鉆孔巖芯的古生物、 ams ~ （ 14 ） c測年、淺地層剖面等，參考qc _ 2 、 dz _ 4成果及標準氧同位素曲線探討了黃東海陸架晚第四紀古環境演化、底棲動物群特徵、古氣候、冰後期以來氣候事件、古水團、沉積速率、古水深、沉積物源、海平面平均上升率，討論目前中國東部海平面上升的狀況、溫室效應及海岸帶保護。And the reefs can be divided into three types : reefs developed in the margin of platform, mud mound in the low slope and patch reefs within the platform
黃泥塘一帶屬紅椿灣邊緣下斜坡的泥丘礁或生物灰泥丘。建7井區、石寶寨、老龍洞等生物礁則屬于臺內點礁。The alteration of wall rock is mainly of propylitization, silicification, carbonatization, argillization and beresitization. the characteristics of alteration show the zoning and overlapping on the space. from the inner to outside of the ore vein zoning is : silicification inner core - argillization - beresitization - propylitization
蝕變在空間上既有分帶性又有相互疊加的特點，其分帶從礦脈中心向外依次為硅化內核?泥化帶?黃鐵絹英巖化帶?青盤巖化帶。In the regions just south of the yangzhi river, farmers cultivated mulberry trees for the leaves on which silk worms fed, as well as tea bushes and a host of other products that created extra resources and allowed for a richly diversified rural economy
淮河以北所種植的蘋果、梨子果肉甜美多汁，大豆、棉花質地絕佳；不過到了十六世紀末，大部分土地已是林木不生，蜿蜒流經平原的黃河河道因夾帶大量泥沙而淤積。For dagang oilfield, cements mainly is calcite, other and fills are mud, silicate, pyrite and organic matter, at least there are two or three stages. ( 4 ). after studying of cement stratagraphy, cementation - dissolution diagenesis is divided into four zones : phreatic, vadose, deep mixing and deep convection zones
從大港探區的實例出發，認為充填物類型除方解石外，泥質充填也較普遍，同時還有硅質、黃鐵礦、有機質等多種充填類型，充填期次至少2一3期; （ 4 ）膠結物地層學研究，將膠結溶蝕成巖作用劃分出四個帶:滲流帶、潛流帶、深部混合帶和深部對流帶。Abstract : because the shenfu - dongsheng mine area is located in intermediate of arid and semiarid zone, its ecological environment is very fragile. based on the fragileeco - environmental, the coal mining and construction have brought out some new environmental problems. man - made debris flow problems is the most serious of them which caused by coal mining, construction of railway and highway as wellas exploiting stone. through a great deal of experiments of artificial simulation setting water rushing to two types of slope debris flow and debris flow gully in shenfu - dongsheng mine site, the characteristics is favourable to formation of debris flow ; ( 2 ) the waste gangue is easy to initiate and is main solid material of debris flow in this area ; ( 3 ) the whole debris flow process could be observed through the model simulation experiment of debris flow gully. at present, this experiment method is the best way to analyze debris flow genesis and process
文摘:神府東勝礦區位於黃土高原北部乾旱半乾旱過度地帶，由於煤田的大量開采，誘發了大量的環境問題，尤以人為泥石流最為嚴重.本文以神府-東勝礦區人為泥石流為研究對象，採用人工放水沖刷模擬實驗的方法，分析了坡面型和溝谷型泥石流源地鬆散體起動、產沙、泥石流過程的特性，所得結論為: （ 1 ）放水歷時長、強度大，有利於泥石流的形成; （ 2 ）棄土石渣易起動，是該區泥石流固體物質的主體; （ 3 ）溝道型泥石流放水沖刷模擬實驗，便於觀測泥石流的全過程，坡面型泥石流放水沖刷模擬實驗，利於統計產沙、觀測侵蝕形態Because the shenfu - dongsheng mine area is located in intermediate of arid and semiarid zone, its ecological environment is very fragile. based on the fragileeco - environmental, the coal mining and construction have brought out some new environmental problems. man - made debris flow problems is the most serious of them which caused by coal mining, construction of railway and highway as wellas exploiting stone. through a great deal of experiments of artificial simulation setting water rushing to two types of slope debris flow and debris flow gully in shenfu - dongsheng mine site, the characteristics is favourable to formation of debris flow ; ( 2 ) the waste gangue is easy to initiate and is main solid material of debris flow in this area ; ( 3 ) the whole debris flow process could be observed through the model simulation experiment of debris flow gully. at present, this experiment method is the best way to analyze debris flow genesis and process
神府東勝礦區位於黃土高原北部乾旱半乾旱過度地帶，由於煤田的大量開采，誘發了大量的環境問題，尤以人為泥石流最為嚴重.本文以神府-東勝礦區人為泥石流為研究對象，採用人工放水沖刷模擬實驗的方法，分析了坡面型和溝谷型泥石流源地鬆散體起動、產沙、泥石流過程的特性，所得結論為: （ 1 ）放水歷時長、強度大，有利於泥石流的形成; （ 2 ）棄土石渣易起動，是該區泥石流固體物質的主體; （ 3 ）溝道型泥石流放水沖刷模擬實驗，便於觀測泥石流的全過程，坡面型泥石流放水沖刷模擬實驗，利於統計產沙、觀測侵蝕形態At dawn, the suspect sought help from hotel staff to move a heavy piece of leather luggage into a taxi. the taxi - driver said that he also helped the suspect move the luggage, weighing possibly in excess of 100 pounds, into another hire - car. it was later confirmed that the suspect had hired a car that same day, and when the car was returned the wheels were covered with mud
酒店職員證實疑犯曾於事發當日與死者在其入住的酒店見面黃昏時份，疑犯請酒店職員幫忙，將一個盛了很重物件的巨型皮箱搬上的士的士司機稱他應疑犯要求協助將大皮箱搬到另一輛出租車上，皮箱極重，相信超過一百磅而租車公司亦證實疑犯于同日租用車輛，交還車輛時輪胎上黏滿泥濘當然，死者頸上纏著的浴袍帶亦屬于該酒店的物品。The next day, the rain had somewhat subsided, and brother hsieh s family returned home. they found that their courtyard had been covered by a layer of yellow mud, but the furniture in the living room was still there ; the mudslide had not carried it away. brother hsieh rushed into his bedroom, and to his great relief, all of master s cds, audiotapes and videotapes lay untouched on the wooden floor
隔天水勢稍退，謝師兄全家回去山上的家，敞開的庭院鋪滿黃泥巴，客廳的傢具都還在，並沒有被土石流帶走，謝師兄沖到臥室查看那些師父開示的cd錄音帶錄影帶等，它們完好如初地放在木質地板上，他的房間一點水都沒有，棉被都是乾的土石流洪水完全避開他的臥室，絲毫都未動一下房內的任何東西！分享友人