oregon

歌曲名:Serenade歌手:Oregon专辑:Best Of The Vanguard Years范逸臣 - Serena词/曲：谭荣健最后一班飞机就要启程了我在曲终人散寻找著快乐我的眼眶哄我别哭了 心却僵冷了这段感情看来已经夭折你就这样用力握著我的手在这双耳朵边轻声说要走我很努力找一个藉口 听觉出了什么错无奈回音却一再强调着你要走Serena 这场战役已分出了胜负 我不服怎么那么快就要俯首臣服 不能哭泪水真的撑得很辛苦 放下吧又觉得事情还没结束Serena 我用幸福交换你的礼物 是孤独还有一场想了很久才能看透的领悟 不认输又得赔上我的全部 再为你祈福Serenahttp://music.baidu.com/song/2709948

forgone interest 应该是被放弃的利息

foregone interest已成定局Taking account of foregone interest, the breakeven price would be$ 58.51.若考虑放弃的利息，盈亏平衡价将达到58.51美元。

portland oregon波特兰俄勒冈双语对照例句:1.RNA networks is located in Portland Oregon and Silicon Valley and is funded by MenloVentures..-----------------------------------如有疑问欢迎追问！满意请点击右上方【选为满意回答】按钮

Oregon Trail[地名] [美国] 俄勒冈小道双语例句1. It was a trading post and stagecoach station on the Oregon Trail in the 1860"s.在19世纪60年代是贸易站和俄勒冈小道上的马车驿站.来自互联网2. An approx 5 mile trail race in Portland, Oregon , on the Wildwood Trail in Forest Park.在俄勒冈波特兰的约5英里小道赛跑,在自然林上, 森林里的小道停车.来自互联网

歌曲名:Sail歌手:Oregon专辑:Music Of Another Present EraIt"s just something to sayKeep going round inside my headI"m gonna save my soulBefore things get impossibleI should have seen the signsThey were right before my eyesHe could have saved my soulI"m falling over cross the bayI think the sun sailed awayNot like those beforeI"m just another body washed up on the shoreThe curse on my bonesHe made a pact rum on the stormsHe could have saved my soulHe could have saved my soulTake me in your armsTake me in your armsTake me in your armsTake me in your armsDo you recall the timeI think you just must have lost your mindAffected by the sunAnother heaven"s lined up as we made our runLet"s stay in the lanesAnd I can barely feel the painI love you so much moreI love you so much moreTake me in your armsTake me in your armsTake me in your armsTake me in your armsTake me in your armsIt"s all done by the painfull skyDenims hung out to dryHow many hours to goBefore the next I say self...Sandstorm remainsI see your angels cross the planeThey never save my soulThey never save my soulTake me in your armsTake me in your armsTake me in your armsTake me in your armsTake me in your armsPactrum on the stormsSave my soulPactrum on the stormsSave my soulPactrum on the stormsSave my soulPactrum on the stormsSave my soulPactrum on the stormsSave my soulPactrum on the stormsSave my soulhttp://music.baidu.com/song/2709928

歌曲名:Sail歌手:Oregon专辑:The EssentialIt"s just something to sayKeep going round inside my headI"m gonna save my soulBefore things get impossibleI should have seen the signsThey were right before my eyesHe could have saved my soulI"m falling over cross the bayI think the sun sailed awayNot like those beforeI"m just another body washed up on the shoreThe curse on my bonesHe made a pact rum on the stormsHe could have saved my soulHe could have saved my soulTake me in your armsTake me in your armsTake me in your armsTake me in your armsDo you recall the timeI think you just must have lost your mindAffected by the sunAnother heaven"s lined up as we made our runLet"s stay in the lanesAnd I can barely feel the painI love you so much moreI love you so much moreTake me in your armsTake me in your armsTake me in your armsTake me in your armsTake me in your armsIt"s all done by the painfull skyDenims hung out to dryHow many hours to goBefore the next I say self...Sandstorm remainsI see your angels cross the planeThey never save my soulThey never save my soulTake me in your armsTake me in your armsTake me in your armsTake me in your armsTake me in your armsPactrum on the stormsSave my soulPactrum on the stormsSave my soulPactrum on the stormsSave my soulPactrum on the stormsSave my soulPactrum on the stormsSave my soulPactrum on the stormsSave my soulhttp://music.baidu.com/song/3469656

Quaternary volcanoes of the Cascade Range form 1200-km-long volcanic arc that extends from southern British Columbia to northern California. The arc is related to subduction of the Juan de Fuca Plate beneath North America. Detailed geologic mapping，measurements of advective heat discharge， and numerous conductive heat flow measurements are available for a 135-km-long section of the Cascade Range in north-central Oregon. This data set allow s us to estimate fluxes of heat and mass ( thermal fluid and magma) and to document the role of groundw ater movement in redistributing heat in the upper crust. The results provide some insight into the thermal structure of the arc，and have implications for its geothermal resource potential.Figure 4. 4. 1 Map showing the location of hot springs，the Quaternary arc，prominent volcanoes ( △) ，the 1500 － m － elevation contour， and the amount of heat transported advectively by the hot spring systems. The total for the southerly group of hot springs ( 26 MW ) is 1. 5 times the value obtained from the individual spring groups ( Table 4. 4. 1) ，because of diffuse input of thermal water into the surface drainage; hot springs: Au，Austin; Ba，Bagby; Br， Breitenbush; Bi，Bigelow ; Be，Belknap; Fo，Foley; Ri， unnamed spring on Rider Creek; Ka，Kahneeta.In the study area ( Figure 4. 4. 1) ， the High Cascades physiographic subprovince is a broad constructional ridge of upper Pliocene and Quaternary ( ＜ 3. 3 Ma ) volcanic rocks surmounted by several Quaternary stratovolcanoes. The High Cascades are flanked by Oligocene to lower Pliocene volcanic rocks of the Western Cascades to the west and Deschutes basin to the east. Western Cascades rocks also underlie the High Cascades; they are generally less permeable than the younger rocks. In this report，we use Western Cascades and High Cascades as location terms. We also distinguish ① the Quaternary ( ＜ 2 Ma) arc，or area of Quaternary vents ( Figure 4. 4. 1) ， because older magmatic heat sources will generally have cooled to near ambient temperatures，and ② the region where uppermost Miocene ( ＜6 Ma) ，Pliocene，and Quaternary rocks are exposed， because their areal extent is roughly coincident with an extensive area of near-zero near-surface conductive heat flow.Most of the thermal springs in the study area discharge in deep valleys in the Western Cascades up to 15 km w est of the Quaternary arc. One set of thermal springs discharges from Oligocene or Miocene rocks 18 km east of the Quaternary arc ( Figure 4. 4. 1) . No thermal springs occur in the Quaternary rocks. With tw o exceptions，the thermal w aters are Na-Cl or Na·Ca-Cl w aters. The ratios of Br to Cl are similar to those in seaw ater; these ratios and the high concentrations of Na and Cl ( Table 4. 4. 1 ) suggest that the thermal w aters may have circulated through rocks deposited in a marine environment. Thermal Na · Ca-Cl w aters are typical of rift zones around the w orld，but in North America occur primarily in the Salton trough and in the Columbia embayment of the Pacific Northw est.Table 4. 4. 1 Geochemical and discharge data for hot springs in the study area* Discharge based on chloride-flux measurements，except for Bagby Hot Spring，where discharge was measured directly.** Discharge temperature. ** * Chemical geothermometer temperatures based on anhydrite saturation，except for Kahneeta and Bagby，which are based on the silica and cation geothermometers. § Combined discharge of Bigelow and Belknap Hot Springs. Dashes indicate lack of data. Hot spring locations are shown in Figure 4. 4. 1.The high Cl content of the thermal w aters makes Cl a useful natural tracer，because surface w aters in the Cascade Range of Oregon contain only about 0. 5 mg / L of Cl. The discharge of groups of thermal springs can be calculated by measuring the increased Cl load of streams passing through hot spring areas. In repetitions done on different occasions，these measurements ( Table 4. 4. 1) have a reproducibility of ± 10% to ± 15% or better，depending on the flow rate of the stream relative to the flow rate of the hot springs and on the Cl concentration in the thermal w ater.Figure 4. 4. 2 Relation betw een deuterium content and elevation for w aters on or w est of the Cascade crest. Deuterium content ( δD) is expressed as D / H ratios in ‰ relative to SMOW ( Standard Mean Ocean Water) . Filled squares are from Na-Cl and Na·Ca-Cl thermal w aters in the Western Cascades. Open squares are nonthermal samples from low -salinity springs and w ells in zero-or first-order ( unchanneled or headw ater) basins on or w est of the Cascade crest，and represent local meteoric w ater. Line is linear least square fit to these data. Because there is little oxygen-18 shift in the thermal waters，δ18O values show a similar pattern.The product of the measured hot spring discharge ( Q ) ，an appropriate density ( ρ) and heat capacity ( c) ，and the difference betw een a chemical geothermometer temperature ( Table 4. 4. 1) and a reference temperature ［Qρc( Tg－ 5℃) ］ gives a measure of the heat transported advectively by the hot spring systems ( Figure 4. 4. 1 ) . The total measured advective heat transport by thermal w ater in the study area is 159 MW ( 159 × 106W ) . For comparison，the Quaternary magma extrusion rate of 3 to 6 km3per kilometer of arc length per million years represents an average heat release of 60 MW to 120 MW in the study area.The isotopic composition of the thermal w aters in the Western Cascades indicates that they w ere recharged at relatively high elevations in the Quaternary arc，if the isotopic composition of precipitation has not changed significantly since the thermal w aters w ere recharged. This w ould be the case if the thermal w aters w ere recharged during the Holocene， as seems likely. The thermal w aters are much more depleted isotopically than local meteoric w aters in the Western Cascades. Their isotopic composition best matches that of meteoric w aters at elevations of 1300 m to 1990 m near the Cascade crest ( Figure 4. 4. 2 ) . The hot springs are at elevations of 500 m to 700 m. Thus an elevation difference of about 600 m to 1400 m drives the thermal circulation systems. The available data suggest that thermal w aters recharged near the Cascade crest circulate to depth and flow laterally for distances of 10 km to 20 km ( Figure 4. 4. 1) before discharging at relatively low elevations in the Western Cascades. Gravitationally driven thermal fluid circulation transports significant amounts of heat from the Quaternary arc into rocks older than 6 Ma and must profoundly affect the pattern of near-surface conductive heat flow. Gravitationally driven flow of low er temperature groundw ater must also transfer heat from the younger rocks to older rocks at low er elevations，but this effect is difficult to measure directly.Conductive heat flow data show that the Quaternary arc and adjacent 2-to 6-million-years- old volcanic rocks constitute a large area of near-zero near-surface conductive heat flow that results from dow nw ard and lateral flow of cold groundw ater ( Figure 4. 4. 3) . In contrast，near- surface conductive heat flow is anomalously high in rocks older than 6 Ma exposed at low er elevations in the Western Cascades ( Figure 4. 4. 4) . A similar pattern of low -to-zero conductive heat flow in permeable volcanic highlands and relatively high heat flow in older，less permeable rocks at low er elevations has been observed in the Cascade Range of northern California.Figure 4. 4. 3 Typical temperature-depth profiles from the Quaternary arc， show ing little or no temperature increase to depths of 150 m or moreFigure 4. 4. 4 Temperature-depth profiles from drill holes collared in rocks older than 6 Ma in the Breitenbush Hot Springs area. The deepest hole w as completed to 2457 m，but w as only logged to 1715 m. The bottom-hole ( 2457 m ) temperature w as higher than 141℃ . The gradient measured over the 1465 m to 1715 m interval ( 31℃ / km) projects to a bottom-hole temperature of 152℃.On the basis of temperature profiles from the Mt. Hood area，New berry Volcano，and this part of the Cascades，the thickness of the nearly isothermal zone in the younger rocks generally ranges from 150 m to 1000 m. In the study area only tw o drill holes collared in Quaternary rocks w ere deep enough that conductive heat flow beneath the nearly isothermal zone could be measured; the values measured w ere 95 mW / m2and 109 mW / m2.The temperature profiles in the Breitenbush area ( Figure 4. 4. 4 ) suggest that the high conductive heat flow measured in rocks older than 6 Ma may be a relatively shallow phenomenon. Seventeen shallow holes ( ＜ 500 m deep ) had high gradients that generally corresponded to heat flow s higher than 110 mW / m2. How ever，a similar gradient in the upper part of the deepest hole ( SUNEDCO 58 － 28) changed abruptly below a zone of thermal fluid circulation at about 800 m depth; that such a change w as observed in the deepest hole suggests that the gradients in the shallow holes are also controlled by groundw ater flow.We have used a heat budget approach ( Table 4. 4. 2) to compare the magnitude of the heat deficit in the rocks younger than 6 Ma with that of the anomalous heat discharge in the adjacent older rocks，and to estimate the magmatic heat input required to account for the total heat flow anomaly. This analysis ( Table 4. 4. 2) is specific to the section of the arc between 44°00"N and 45°15" N. The regional heat flow map used in our analysis is shown as Figure 4. 4. 5. The conductive components of the budget are defined relative to assumed background heat flow values and are obtained by measurement of areas on Figure 4. 4. 5 with a planimeter. In general，heat flow in a given area is taken as the average of adjacent contours ( for example，70 mW / m2 between the 60 mW / m2and 80 mW / m2contours) . We assigned values of 140 mW / m2within the 120 mW / m2contours and 60 mW / m2outside the 80 mW / m2contours east of the Quaternary arc.Table 4. 4. 2 Components of the heat budget ( in MW)* Based on discharge temperatures. The difference between the geothermometer and discharge temperatures is due to conductive heat loss and，particularly in the Western Cascades，represents a significant fraction of the conductive anomaly.Important assumptions in the heat budget analysis are as follow s: ① The background conductive heat flow beneath the isothermal zone in the Quaternary arc is 100 mW / m2. This value is typical of areas of Quaternary volcanism and is consistent w ith the tw o measurements in the study area. ② The background heat flow in Tertiary terrane is 60 mW / m2. Values over 60 mW / m2are the result of tectonic，magmatic，radiogenic，or hydrologic sources. ③ The heat output of the hot springs represents the anomalous，advective heat discharge from rocks older than 6 Ma. This is a minimum value because it does not include low er temperature advective discharge，w hich is difficult to measure.The values for hot spring heat output used in the budget are based on discharge temperatures ( Td) rather than the geothermometer temperatures ( Tg) used previously to calculate advective heat transport. The difference between Tgand Td( Table 4. 4. 1) results from conductive cooling and presumably appears as part of the conductive anomaly. In the Western Cascades，the thermal power represented by the difference between Tgand Td( 67 MW) is equal to about half of the conductive anomaly ( compare the values in Figure 4. 4. 1 and Table 4. 4. 2) .The area of near-zero near-surface conductive heat flow in this part of the Cascade Range is generally coincident with the areal extent of permeable volcanic rocks younger than 6 Ma. On the basis of our assumptions regarding background heat flow ，about 460 MW of heat are swept out of these younger rocks between 44°00"N and 45°15"N by groundwater circulation. This amount is roughly balanced by about 350 MW of anomalous heat discharge in the rocks older than 6 Ma ( Table 4. 4. 2) . Apparently，sufficient heat is removed advectively from the rocks younger than 6 Ma to account for the anomalous heat discharge on the flanks of the Cascade Range. The difference betw een the heat deficit in the younger rocks and the anomaly in the older rocks ( about 110 MW) may occur as lower temperature advective discharge， which was not determined directly. The difference between the heat deficit in the younger rocks and the heat ( Tg) transported advectively by the hot spring systems ( 460 － 160 = 300 MW) is an estimate of the heat removed from the younger rocks by low er temperature groundw ater flow or by yet- unidentified thermal fluids.Figure 4. 4. 5 Map show ing lines of equal heat flow. Area of near-zero near-surface conductive heat flow rocks younger than 6 Ma is diagonally hatched. This area is estimated conservatively; w e have included in it all areas w here rocks younger than 2 Ma are exposed but only included areas w ith rocks betw een 2 and 6 million years old w here temperature profiles indicate that conditions are near isothermal. Areas of silicic volcanism in the Quaternary arc are show n in region. Names of hot springs are on Figure 4. 4. 1. The heat flow contours are based on 253 temperature profiles，101 of w hich have also been previously published and interpreted.Because the anomalous heat discharge in the older ( ＞ 6 Ma) rocks can be explained in terms of advection from the younger rocks， w e ne

是美国俄勒冈州比弗顿耐克服装公司。总部位于美国俄勒冈州Beaverton的耐克公司是全球著名的体育用品制造商。该公司生产的体育用品包罗万象：服装，鞋类，运动器材等等。2002年，公司的营业收入达到了创纪录的49、8亿美元，比2001财年增长2%。耐克公司用自身骄人的业绩印证着其创始人比尔_鲍尔曼曾说过的一句话："只要你拥有身躯，你就是一名运动员。而只要世界上有运动员，耐克公司就会不断发展壮大。

尤金俄勒冈州（美国）

歌曲名:Violin歌手:Oregon专辑:The EssentialVIOLIN|AZU作词：AZU作曲：AZU & KAZUHIKO MAEDA溢れる気持ち押しころして胸に闭じ込めたまま　眠る夜これ以上踏み込んじゃダメ…と分かっててもI MISS YOU...BABYI"LL BE BESIDE YOU気づいてよ　分かってよ　言えない想い重ね合う时だけが増えて奥に闭じ込めて　愿いかけて…信じて眼に映るものを受け止めて　私を见て弱くて儚いこの心は暖かいあなたの手に触れられぬまま涙さえ流せずに强いふりしてるの?OH BABY WHY?OH BABYBUT I CAN"T STOP LOVING YOU悩んでも　迷っても　あなたがいい叶わぬ恋があるとしても声も　ぬくもりも　やさしいから见つめて眼に映るものを受け止めて　ただそばにいて気づいてよ　分かってよ　言えない想い重ね合う时だけが増えて奥に闭じ込めて　愿いかけて…信じて眼に映るものを受け止めて　私を见て悩んでも　迷っても　あなたがいい叶わぬ恋があるとしても声も　ぬくもりも　やさしいから见つめて眼に映るものを受け止めて　ただそばにいておわりhttp://music.baidu.com/song/3469651