沟滩

基本解释 (translations)

vadum

与沟滩相关的网络例句 [注：此内容来源于网络，仅供参考]

Since the largest Ta'ergou tungsten deposit in northwest China and Sh idonggou argentum multi-metal deposit were discovered, the Yeniutan granite in Subei county Gansu province is even more famous.

摘 要：位于甘肃省肃北县的野牛滩岩体，因产有中国北方最大的塔儿沟钨矿以及新发现石硐沟银多金属矿而著名。

The high porosity zone occurrence of the Tertiary reservoir composed of clastic rocks in the Yuanyanggou region is controlled by diageneses and sedimentary facies, lying in the early diagenetic stage A ~ the late diagenetic stage A1 and the area of the sandstones developing in debouch bar, braided-divided flow channel, raised bank and channel bar is namely high porosity zone development of the lower Shasan Member (Es33) and the upper-middle Shasan Member (Es31-2); furthermore, lying in the late diagenetic stage A2 and the area of the sandstones developing in debouch bar, braided-divided flow channel, raised bank and channel bar is namely high porosity zone comparative development of the lower Shasan Member (Es3) and the upper-middle Shasan Member (Es31-2), the physical property of the reservoir is relatively worse.

鸳鸯沟地区第三系碎屑岩储层高孔带分布受成岩作用和沉积相的控制，处于早成岩阶段A期～晚成岩阶段A_1期，且有河口坝、辫状分流河道、天然堤和心滩沉积微相砂体发育的区域即为该区沙三下亚段和沙三中上亚段储层高孔带的发育区；而处于晚成岩阶段A_2期，且沉积相也为河口坝、辫状分流河道、天然堤和心滩沉积微相砂体发育的区域即为鸳鸯沟地区沙三下亚段和沙三中上亚段储层高孔带的较发育区，储层物性相对较差。

The basal geomorphology structure of the Tidal-Basin System of the Tiaozini Sandbanks is watershed and tidal creek system. We analyses its formation, evolvement, geomorphology characters and development and discusses the main influence factors which is water, sediment and space. We divide the evolution phases which is formation phase, autumn phase and contabescence phase. In the end we confirms its main functions, which is discharging the folium water on the tidal flat of the Tidal-Basin in the end of the ebb-tide, transporting sediment to Tidal-Basin through tidal creek systems, confining the swing range of the dynamical axis of flood tide or ebb tide, balancing the dynamical status of the South and North. At the same time, we compare coastal tidal-basin and sandbanks tidal-basin on geomorphology characters, formation causes, style and so on.

条子泥潮盆—潮沟系统的基本地貌结构为分水滩脊和潮沟系统，本文分别对它们的形成与发育、地貌特点及动态变化进行了分析，并探讨了影响其发育的主要因素，即来水条件、来沙条件、空间条件，划定了其主要发育阶段，即形成期、成熟期、衰亡期；在上述分析的基础上确定了潮盆—潮沟系统的主要功能，即通过潮沟系统渲泄落潮后期滞留在其潮盆范围内的滩面薄层水、通过潮沟系向潮盆内部输入或输出泥沙、限制涨落潮动力主轴摆动范围、平衡南北两侧动力状态；同时针对岸滩潮盆—潮沟系统与沙洲潮盆—潮沟系统的地貌特征、成因类型等进行了对比分析。

There are Shuzheng area, 75 km long, Bonsai Beach, Hoi Kwan Shu Zheng, Shu Zheng falls, sea dragons, sea sparks, component Wolonghe sea, and other attractions; days ditch area, on Long Hospital, Pearl Beach, High Falls of the three major falls, sea-, Xiong Maohai, Sea Grass, Sea Swan, Yan Jian, primeval forest, hanging-chuen, Wu Huahai, and other attractions; Zechawagou area, 75 km long and Wucai Chi Changhai , And other attractions; such as the bar area, rock devil, such as the Temple bar, and other attractions.

主要有树正景区，长75公里，有盆景滩、树正群海、树正瀑布、双龙海、火花海、卧龙海等景点组成；日则沟景区，有诺日朗、珍珠滩、高瀑布三大瀑布，有镜海、熊猫海、芳草海、天鹅海、剑岩、原始森林、悬泉、五花海等景点；则查洼沟景区，有长75公里的长海和五彩池等景点；扎如景区，有魔鬼岩、扎如寺等景点。

Village committee jurisdiction: Angulinao黄盖West yingzi, small groove big groove Well, big business Gou, West Dajing, Hao camp,田官Square,石沟war, the East slope, double love together, small Grein, North Beach , SU, Lin Yuan, mouth Shan, meaning together, Fu River, He Jiali yingzi.

辖19个村委会：黄盖淖、西营子、小井沟、大井沟、大苟营、西大井、郝家营、田官坊、战石沟、东山坡、双爱堂、小格赖、北滩、东坡、林源、口山、义合、富河、贺家营子。

It is understood that the two newly discovered rock paintings located in the town ofsan yan jing Village Shawodi Tulipa Red Cliff and the village of West Town, the original pine bifurcated Bay, This is the second team in the 2007 census Town of ginger red JINWOZI trenches, in Stephen Township shape of the groove, pull the card right Township ditch, temple paintingstan xiang deer then ditch the newly discovered ancient rock paintings.

据了解，新发现的两处岩画分布于上沙窝镇三眼井村老鸦崖和红水镇原松林村西岔湾，这是继2007年普查队在红水镇的姜窝子沟、中泉乡的板形沟、正路乡的拉牌沟、寺滩乡的画鹿沟之后又新发现的古代岩画。

The south-north united tectonic environment and tectonic pattern does not exist. The east-west trend thrusting Nappe structure of Majiatan and Hengshanpu can not represent the whole western margin of Ordos. The attempt to solve the regional tectonic problem with simple tectonic pattern is against the geological theory, especially in the Helan Mountain region.(2) After the geochemical data analysis of Ruqigou basalt in Helan Mountain, the article illustrates that it belongs to continental rift basalt which appeared in the late-Triassic and early middle Jurassic. Meanwhile the article states that the region is located in the rift environment of an extension background and Rudigou is located in the central part of the rift.(3) The article illustrates that the western ridge of Helan Mountain used to be on a slope and topography slowly declines from west to east after analysis and demonstrations of the distribution under XiaoSongshan bedding fault. Through comprehensive analysis of the no-strong deformation and bedding fault features, the article states that the Xiaosongshan bedding fault used to be gravity slip detachment structure and it represents the extension from the east to the west. Based on the above and analysis and demonstrations of isotope age and track datting, the article illustrates that the ? characteristic of the east of the western ridge of Helan mountain being higher than the west is the result of its late tectonic reverse.(4) Through comparison between Rujigou region Mesozoic Era late Triassic period-early and middle Jurassic period deposit and that of Ordos Basin and the analysis of the late Triassic period extension and early -middle Jurassic Period deposit povenevance it sets forth that during the period, Rujigou region was part of a large deposit basin which was closer to the northern povenevance and farther from the western povenevance.

以马家滩和横山堡为代表的东西向逆冲推覆构造模式，在整个鄂尔多斯盆地西缘不具有全区统一性，那种试图用单一的构造模式解决本区构造问题的尝试，无疑是与地质实际相悖的，尤其是对贺兰山地区；(2)通过对贺兰山汝箕沟玄武岩地质地球化学测试分析，提出其为大陆裂谷玄武岩，其形成时代为晚三叠—早中侏罗世，并通过该玄武岩的稀土和微量元素的测试分析资料进行了多种判别分析，最终确定该区处于拉张背景下的裂谷环境，汝箕沟地区大致处于当时裂谷的中心部位；(3)通过对小松山断层面之下地层分布规律，结合其变形特征的分析论证，认为当时贺兰山西麓处于一个由东向西平缓抬高的斜坡环境，并通过小松山断层面之下地层的非强烈变形及顺层断层特征等的综合分析，认为贺兰山西麓的小松山断层原本是一重力滑覆断层，它代表了近东西向的拉张，在此基础上通过裂变径迹测试资料的分析论证对其做了进一步认定，目前贺兰山西麓东高西低的剖面特征是该区后期构造反转的结果；(4)通过对汝箕沟地区中生代晚三叠世—早中侏罗世沉积与鄂尔多斯盆地内部的对比、晚三叠世延长组及早中侏罗世沉积物源和水流向分析，认为该时期汝箕沟地区为一更靠近北部物源，而距西部物源明显较远的沉积环境，是一更大型沉积盆地的一部分。

Gray-brown desert soil in 1300-2400 meters above sea level red-Bay, ditch grass, the East mountains, I-Ping Xia, sand pool flood channel, the first Dragon Hill, Hill throttle, the stockade Beach, Beach Niangniang Temple, Kowloon Bay dam, Dongtan, the next quarter of the beach, two Shagou, wild rivers, indiscriminate block Beach and other places, a total of 437.16 million.

灰棕漠土分布在海拔1300-2400米处的红湾子、草沟、东大山、平口峡、沙涝池沟、龙首山、风门山、大寨子滩、娘娘庙滩、九坝滩、东滩、下四分滩、两分沙沟、野河、乱墩子滩等地，共437.16万亩。

As a sensitive belt of sea and land interaction, silt tidal flat is characterized as muddy surfaces, densely covered and frequently varied inlets. Therefore, the routine topography survey method has been greatly restrained.

淤泥质潮滩作为海陆相互作用的敏感地带，滩面泥泞、潮沟密布、变化频繁，常规的地形测量难度极大。

The basal geomorphology structure of the Tidal-Basin System of the Tiaozini Sandbanks is watershed and tidal cr...

条子泥潮盆-潮沟系统的基本地貌结构为分水滩脊和潮沟系统，本文分别对它们的形成与发育、地貌特点及动态变化进行了分析，并探讨了影响其发育的主要因素，即来水条件、来沙条件、空间条件，划定了其主要发育阶段，即形成期、成熟期、衰亡期；在上述分析的基础上确定了潮盆-潮沟系统的主要功能，即通过潮沟系统渲泄落潮后期滞留在其潮盆范围内的滩面薄层水、通过潮沟系向潮盆内部输入或输出泥沙、限制涨落潮动力主。。。

与沟滩相关的网络解释 [注：此内容来源于网络，仅供参考]

swashway：沙滩沟道

沙滩,海滩,湖滩 beach | 沙滩沟道 swashway | 沙岩 sandstone

swash channel：滩间水道

"沙洲航漕,冲击滩","swash" | "滩间水道","swash channel" | "沙滩沟道","swashway"