An example of River - Ocean Interaction Zone: The Fluviotidal Channel in Estuarine System, a Facies Model with Climbing Ripple Bedding

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An example of River - Ocean Interaction Zone: The Fluviotidal Channel in Estuarine System, a Facies Model with Climbing Ripple Bedding

机译：河流-海洋相互作用带的一个例子：河口系统中的潮汐河道，一种具有波纹状河床的岩相模型

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《Geo-Eco-Marina》 |1997年第2期|共5页
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中图分类地质学;
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1. Rhythmic Climbing-Ripple Cross-Lamination in Inclined Heterolithic Stratification (IHS) of a Macrotidal Estuarine Channel, Gomso Bay, West Coast of Korea [J] . Kyungsik Choi Journal of Sedimentary Research . 2010,第6期

机译：韩国西海岸Gomso湾巨潮河道斜异层分层（IHS）的节律性爬升-波纹交叉分层
2. Rhythmic climbing-ripple cross-lamination in inclined heterolithic stratification (IHS) of a macrotidal estuarine channel, Gomso Bay, west coast of Korea [J] . Choi K. Journal of sedimentary research . 2010,第5a6期

机译：韩国西海岸Gomso湾巨潮河口河道斜异质层状分层（IHS）中的节律性攀爬-波纹交叉层压
3. Tidal-Fluvial and Estuarine Processes in the Lower Columbia River: II. Water Level Models, Floodplain Wetland Inundation, and System Zones [J] . Jay David A., Borde Amy B., Diefenderfer Heida L. Estuaries and coasts . 2016,第5期

机译：下哥伦比亚河的潮汐河口和河口过程：II。水位模型，洪泛区湿地淹没和系统区域
4. A Geomechanics Driven Facies Model to Reconcile Production, Inform Completion Strategies, and Determine Landing Zones in the Green River Basin [C] . Joel Mazza, Jesse Havens, Torrey Mullen SPE/AAPG/SEG Unconventional Resources Technology Conference . 2019

机译：地质力学驱动的相模型可以协调生产，告知完成策略，并确定绿河流域的着陆区
5. A sedimentologic and ichnologic facies model for mud-dominated inner-estuarine deposits, Mary's Point and the Shepody River, Bay of Fundy, New Brunswick, Canada. [D] . Pearson, Nadine Jennipher. 2006

机译：加拿大新不伦瑞克省芬迪湾的以泥浆为主的内河口沉积物，玛丽角和谢波底河的沉积学和岩石学相模型。
6. Chesapeake Bay nitrogen fluxes derived from a land‐estuarine ocean biogeochemical modeling system: Model description evaluation and nitrogen budgets [O] . Yang Feng, Marjorie A. M. Friedrichs, John Wilkin, -1

机译：切萨皮克湾的氮通量来自陆地河口海洋生物地球化学模拟系统：模型描述评估和氮预算
7. Figure 5: (A) SW view of a meseta on the background, taken from the A19 road; (B) amphitheatre outcrop (Tz 21), preserving Cenozoic reddish deposits over older sequences; (C) outcrop along the Muhuesi river (Tz 36), with cross trough stratified sandstones of the Mahogo Formation; (D) river bank outcrop north of the Muhuesi river (Tz 44) with calcretes in the Mbaragandu Formation; (E) outcrop along the Lukoswe river (Tz 40) with stratified sandstones (Mkuju Formation) over massive mudstones (Mbaragandu Formation); (F) carbonate concretions in the Mbaragandu Formation (Tz 43); (G) outcrop at the Zinzima river (Tz 18), with laminated mudstones, with climbing ripples; (H) outcrop along the Mkundi river (Tz48), with low-angle stratified sandstones of the Mkuju Formation over the massive mudstones of the Luwegu Formation. [O] . -1

机译：图5：（a）在背景中的一个meseta的Sw视图，从A19路上采取; （b）圆形剧场露头（TZ 21），在较老序列中保留新生代红沉积物; （c）沿着Muhuesi River（TZ 36）的露出，带有Cross Trough的摩托摩擦砂岩; （d）河北河畔北京北部（TZ 44），曼加大学的群体; （e）沿着卢克韦河（TZ 40）露出巨大的砂岩（MKUJU形成）在大规模的泥岩上（Mbaragandu形成）; （f）Mbaragandu形成中的碳酸盐凝固（TZ 43）; （g）Zinzima River（TZ 18）的露出，带有层压的泥岩，具有攀爬涟漪; （h）沿着Mkundi河（TZ48）露出，用MKUJU的低角度分层砂岩形成，在陆扣式泥土形成的巨大泥岩上。
8. MIZEX. A Program for Mesoscale Air-Ice-Ocean Interaction Experiments in Arctic Marginal Ice Zones. III. Modeling the Marginal Ice Zone [R] . Hibler, W. D. 1984

机译：mIZEX。北极边缘冰区中尺度气 - 冰 - 海相互作用实验程序。 III。边缘冰区建模

An example of River - Ocean Interaction Zone: The Fluviotidal Channel in Estuarine System, a Facies Model with Climbing Ripple Bedding

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