I noticed the Sun setting in the NNW location. I haven't been able to observe the sunrise.
我注意到太阳在西北方向偏北的位置，我还没有看见过日出。
On the eastern side of the north region lies the northwest Yunnan extensional taphrogenic belt, which is characterized by three sets of rift type faulted basins striking NNW
上述变形特征反映在构造地貌上为北部盆岭构造、中段线性断谷断盆构造及南部压性盆地变形，其中苍山—洱海一带断裂两侧主夷平面的巨大落差是红河断裂上新世以来断陷正断作用的显著代表。
The evolution process under the control of the multigeodynamic force system (including the boundary forces of Eurasia-Pacific-Indian three massive plates around Nansha block, effects of the deep mantle, relative soft layer-sliding planes within Nansha lithosphere block and the earth's rotational inertial force) can be briefly divided four stages: the late Cretaceous to the early Eocene stage of uprilfing-erosion and shear-extension caused by the oceanwards-eastwards withdrew of Pacific subduction zone and the delamination of proto-subducted slab after the stage of pre-Cretaceous pre-rifting active continentoceanic plate margin. In this stage, the Nansha transcrustal layering-block started to move southeastwards on the Nansha transcrustal layer-sliding plane, meanwhile, the Andu-Bisheng and Liyue-Banyue basement layering-block slid on their upper-crust layer-sliding planes, and Xibu accretion zone was formed. Successively, it entered the stage of the mid-Eocene to early Oligocene, when NW-SE sea-floor spreading occurred in the southwest subbasin owing to the slip-line field initiated by the collision between the Indian and Eurasian plates, Zengmu foreland-basin started to develop in the same time. And in the stage of late Oligocene to early Miocene, near NS simple-shear extension and sea-floor spreading in the central subbasin of eastern South China Sea resulted from the south-southeastwards drawing-force of the mantle-flow. The crustal layering-blocks and the Miri accretion zone formed also in this stage.
南沙岩石圈新生代微板块及板内层块构造的动力演化过程，在多元动力等因素(如块体之外的欧-太-印三大板块运动边界力和地幔深部活动因素、块体内部软弱层滑面以及地球自转变化)控制下，大致经历了4个阶段的演化：从前晚白垩世的裂前活动陆-洋板块边缘阶段因太平洋俯冲带向东跃迁、原向NNW俯冲消亡的板片的拆沉、幔隆而进入晚白垩世-早始新世的隆升剥蚀、剪切伸展演化阶段，南沙超壳层块顺超壳层滑面祥东南运移、安渡-毕生与礼乐-半月基底层块沿上壳层滑面拆离，西布增生带形成；继而先后在中始新世-早渐新世期间受印-欧板块碰撞滑线场、地球自转加速影响出现西南海盆NW-SE向海底扩张和曾母前陆盆地的发育，和晚渐新世-早中新世期间南—东南向地幔流牵引造成的中央次海盆近NS向单剪伸展与海底扩张、壳体层块向南差异滑移、米里增生带形成；中中新世以来，印度-澳洲板块快速向北俯冲，构成今日南海格局。
While under Port Columbus International airport civilian radar approach control at 15 miles out and descending through 8, 000 feet I was given permission to vector 30 degrees right to investigate what appeared to be a 2nd sun about 2/3 the size of a football field parked on the back side of a large cumulous cloud at about 4, 000 feet and 5 miles NNW of the airport.
当在哥伦布港口国际机场民用雷达15英里作用半径外和慢慢通过8，000英尺我得到无线电许可要求向右转30度去调查在飞机场的4，000英尺和5英里NNW的大约是2/3足球场大小大积云状的云层后面停留的第二个太阳。
Xiaozhongdian Basin is a NNW-directed fault depression basin which was shaped while the Qinghai-Tibet Plateau intensely upheaved since the end of the Pliocene epoch, where the lacustrine clay of the middle and late Pleistocene is well distributed from the Xiaozhongdian River section.
滇西北小中甸盆地是上新世末期以来在青藏高原强烈隆起过程中形成的NNW向第四纪断陷湖盆地，从深切的小中甸河谷剖面可见盆地上部发育中晚更新世湖相粘土。
The Huade Group underwent at least two phases of deformation:the early phase of deformation gave rise to ENE-trending synclinorium and the late phase was marked by tectonic superimposition, forming NNW-trending folds. The main phase of deformation likely occurred in ~2.0 Ga B. P. The deformation of the Huade Group is related to a Paleoproterozoic orogenic event along the northern margin of the North China Craton, which has great significance for the study of accretion and breakup of the North China Craton.
化德群经历了两期构造变形，早期为北东东走向的复式向斜，晚期又遭受了构造叠加，形成了北北西向褶皱构造，其主期变形可能发生在2.0 Ga左右，它的褶皱造山是华北克拉通在古元古代向北增生的体现，这对研究华北克拉通的增生，裂解具有重要意义。
The sandstone of reservoir spreads NNW-NW. The high thickness of sandstone develops in northwest and center of the study area, and it changes thinner to dactylitic pinchout in the direction of southeast.
砂岩总体走势北北西～北西向，砂岩厚度高值区发育在研究区西北部和中部，向东南方向砂岩有逐渐变薄直至指状尖灭的趋势。
The results indicate that the study area can be partitioned into four seismic belts or regions, namely the Sea of Japan to Changbai Mountains deep seismic belt, the northern Tanlu Fault seismic belt, the western margin of Songliao basin seismic belt and the inner Songliao basin seismic belt. The seismic activity of the northern Tanlu Fault zone is weak and inhomogeneous. The Yilan-Yitong Fault is more active than the Dunhua-Mishan Fault, and shows segmentation behavior that is stronger at both sides than the middle part. The maximal stress axis in the deep seismic belt trends 288° on average, dipping 31° and the main fault movement mode is reverse. Near the northern Tanlu Fault zone the P-axis mainly trends NEE-SWW, dipping 26° on average, the T-axis mainly trends NNW-SSE, dipping 23° on average and the main fault movement mode is strike-slip with reverse.
结果表明，郯庐断裂带北段及邻区的地震活动可分为日本海－长白山深震区、郯庐断裂带北段地震区、松辽盆地西缘地震区和松辽盆地内部地震区；郯庐断裂带北段现今地震强度较小，频度较低，但空间差异性显著，依兰－伊通断裂活动性比敦化－密山断裂强，且具有两端强而中间弱的分段活动特点；深震区P轴平均走向为288°，倾角约31°，断裂活动以逆断为主；郯庐断裂带北段附近浅震P轴走向以NEE-SWW向为主，倾角平均26°，T轴走向以NNW-SSE向为主，倾角平均23°，断裂活动以走滑和逆断为主。
At 20 HKT, SINLAKU was centred about 80 km (40 NM) NNW of Taipei.
在 20 HKT，森垃克集结在台北之西北偏北约 80 公里(40 海里)。
At 20 HKT, 02W was centred about 180 km (100 NM) NNW of Yap.
在 20 HKT，02W 集结在雅葡岛西北偏北约 180 公里(100 海里)。
These dust events were characterized by about 1-3 day duration, and NNW, NW, WNW.
而每逢降雨增加时，在之后的1～3年内，出现降尘的高峰期。
The newly formed Tengchong-Jinghong NNW zone and Dali-Chuxiong NWW zone have an important role in the block division.
指出新生的腾冲-景洪北北西带和大理-楚雄北西西带在活动地块划分中的重要作用。
NEOGURI continued to move NNW in the past 12 hours, maintaining intensity in the meantime.
浣熊於过去 6 小时维持强度并持续向西北偏北移动。
The authors have analysed the transmissivity using the dominant surface theory and concluded that 1 the Hanqiao F1 is a waterrich dominant surface, 2 the Hanqiao F1 along with the NNW w.
本文应用新构造优势面理论分析其导水性，认为韩1号断层是一条富水优势面，并和NNW向的新构造富水优势断裂组成该处地下水运移的网络通道，在韩1号断层带处一旦揭露NNW向断裂，就可能发生突水事故，将该结论用于封堵韩1号断层突水方案的选择，取得了理想的效
It is concluded that the existence of NNW-SSE crevice in salt stratum is the fundamental reason for successful fracturing and communication modification K series brine well.
该矿区含盐地层中NNW-SSE向断裂裂隙的存在是K系列卤井压裂连通改造成功的根本原因。
Generally, the direction of Eogene stress fields in Machang Area had swinged from NWW-SEE to NNW-SSE.6. This paper also discussed the relationship between the transition structures and hydrocarbon accumulation.
马厂地区新生代古近纪的主拉张应力场方向具有NWW-SEE方向至NNW-SSE方向来回摆动的特征。6、利用研究区各断裂体系所起作用不同，通过变换构造及伸展区三维构造研究，对研究区的油气成藏规律及控制因素进行了有益的讨论，对研究区油气勘探有一定的指导意义。
Chaijiazhuang gold mine located in Lizhiyuan-Diaobazhi gold ore deposit belt that belong to North Qinling Caledonian folded belt of West Qinling folded system and hosted in Danfeng Group that belong to exocontact of Chaijiazhuang adamellite.
柴家庄金矿位于西秦岭褶皱系北秦岭加里东褶皱带李子园—吊把子金矿带上，赋存于柴家庄二长花岗岩体外接触带的丹凤群地层中，严格受NE向及NNW向断裂控制。
In Late Jurassic period (159-135Ma), when the orientation of maximum principal compressive stress was NW direction, the Wuzhangshan granite intruded to upward, accompanied the formation of NW trending Sanrenchang and Huangshuian breccia pipe belts; In the Early Cretaceous period (135-120Ma), when the orientation of maximum principal compressive stress was NNW trending, the second stage of Huashan granite intruded to upward, accompanied the formation of NW trending Qiyugou breccia pipe belts; In 120-105 Ma, when the orientation of maximum principal compressive stress changed to NE direction, the gold-bearing quartz veins and gold orebodies in breccia pipes were formed along the NE trending fractures; In the Middle Cretaceous period (105-85 Ma), when the orientation of maximum principal compressive stress was NEE, the NEE trending Leimengou granite porphyry intruded to upward, accompanied the formation of NEE trending Leimengou breccia pipe belts.
在晚侏罗世(159～135Ma)，构造应力场最大压应力方向为NW向，形成了NW走向的五丈山岩体以及NW向展布三人场、黄水庵两个角砾岩带；在白垩纪早期(135～120Ma)，最大压应力为NNW向，形成了花山岩体第二期上侵，并伴有NW向的祁雨沟角砾岩带；其后(120～100Ma)，构造应力场最大压应力方向变为NE向，形成了NE向含金石英脉及角砾岩体中金矿体；最后(100～80Ma)，形成了雷门沟花岗斑岩以及NEE向展布的雷门沟-杨河沟角砾岩带(区域构造应力场的最大主压应力方向为NEE向)。
DOLPHIN should decelerate and move N to NNW along the western periphery of the subtropical ridge.
白海豚将沿副热带高压脊西面向北或西北偏北移动，移速将会减慢。
There is a high P wave velocity anomaly striking NNW at the depth of 12km under the earthquake swarm area. It extends downwards to the depth of 16km at least, and is surrounded by relatively low velocities. V/V ratios are also characterized by high values in this region. This kind of structural differences may be related to the occurrences of Jiashi strong earthquake swarm.
自12km深度开始，在与强震群震中相应的位置上，明显出现沿北北西向的高P波速度异常体，在其周围为相对低速分布，呈现出低速条带环绕高速条带的分布格局，V/V在相同的位置上也表现为高值分布。