標(biāo)題: Titlebook: Atlas of the Deep-Water Seabed; Ireland Boris Dorschel,Andrew J. Wheeler,Koen Verbruggen Book 2010 Springer Science+Business Media B.V. 201 [打印本頁(yè)] 作者: 導(dǎo)彈 時(shí)間: 2025-3-21 16:46
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作者: 廢除 時(shí)間: 2025-3-21 20:43 作者: 分發(fā) 時(shí)間: 2025-3-22 02:29 作者: capillaries 時(shí)間: 2025-3-22 05:53
Below the Irish Seabedthat Pangea started to split apart creating a series of rift valleys. Eventually, this rifting split all the way through the continental crust and a new ocean basin was formed with two new smaller continents on either side: the North Atlantic, Europe and North America respectively. The gross morphol作者: 上下倒置 時(shí)間: 2025-3-22 10:56 作者: 臭了生氣 時(shí)間: 2025-3-22 13:25
Above the Irish Seabedmasses occurring at distinct water depth intervals. As a result of this stratification, the water in the ocean can flow in different directions at different depths. Individual water-masses can be characterised by their physical properties with the temperature and salinity (concentration of salt in s作者: 不容置疑 時(shí)間: 2025-3-22 20:57 作者: prostatitis 時(shí)間: 2025-3-23 00:46 作者: epicardium 時(shí)間: 2025-3-23 01:34
Escarpmentsting. The specific reasons why escarpments form on the seabed can be many fold (although faulting is no longer an active process on the Irish margin). Escarpments can form as a result of strong, slope-parallel bottom currents, or as the scars left following submarine (land)slides. In addition, they 作者: 合乎習(xí)俗 時(shí)間: 2025-3-23 06:22 作者: white-matter 時(shí)間: 2025-3-23 10:52 作者: Engaged 時(shí)間: 2025-3-23 17:21 作者: 緩和 時(shí)間: 2025-3-23 20:04
Porcupine Seabighton years ago. It is bordered by the Slyne Ridge in the north, the Porcupine Bank in the west and the Goban Spur in the south. The Porcupine Seabight opens to the southwest onto the Porcupine Abyssal Plain. Water depths in the Porcupine Seabight range from approximately 400 m in the north to 3,000 m 作者: 法律的瑕疵 時(shí)間: 2025-3-23 23:19 作者: indignant 時(shí)間: 2025-3-24 02:22
Northernmost Irish Continental Margins the northern extension of the eastern margin of the Rockall Trough. In its southern and central part, the northernmost Irish continental margin is characterised by relatively steep slopes and numerous canyon systems. Only in the very northern part do slope angles gradually decrease and there the m作者: Thyroiditis 時(shí)間: 2025-3-24 08:58
Rockall Troughnorthernmost Irish continental margin in the east and the Rockall Bank in the west. The Rockall Trough opens onto the Porcupine Abyssal Plain to the south (Fig. 16.1). Like the Porcupine Seabight, the Rockall Trough also evolved during the opening phase of the Atlantic starting 250 million years ago作者: avulsion 時(shí)間: 2025-3-24 14:21 作者: 不利 時(shí)間: 2025-3-24 18:21 作者: 沙草紙 時(shí)間: 2025-3-24 22:20 作者: 閹割 時(shí)間: 2025-3-24 23:25 作者: cancellous-bone 時(shí)間: 2025-3-25 05:02 作者: 新陳代謝 時(shí)間: 2025-3-25 09:01 作者: Angiogenesis 時(shí)間: 2025-3-25 13:53
Escarpments Escarpments can form as a result of strong, slope-parallel bottom currents, or as the scars left following submarine (land)slides. In addition, they can be associated with morphological features such as canyons and seamounts. Regardless of the formation processes, escarpments are the results of erosive processes active on the continental slope.作者: 發(fā)芽 時(shí)間: 2025-3-25 18:36
Below the Irish Seabedogical structures of the Irish deep-water seabed developed as a result of a series of rift valleys that formed during the early development of the north Atlantic starting in the Permo-Triassic geological period (around 250 million years ago).作者: 弄臟 時(shí)間: 2025-3-25 20:30
Porcupine Seabightat its mouth in the southwest. The northern border of the Porcupine Seabight is difficult to define with no clear break of slope but a gradual transition from the Seabight to the Porcupine Bank and Celtic Shelf. With the borders as presented here, the Porcupine Seabight covers an area of 67,100 km. (Fig. 13.1).作者: Anal-Canal 時(shí)間: 2025-3-26 01:56
Rockall Bankvel. Being separated from the Irish continental margin by the Rockall Trough, the Rockall Bank represents a relatively sediment starved area isolated from the input of terrestrial sediments by rivers and glaciers. Morphologically, the Rockall Bank is characterised by a generally steeper eastern slope and a generally gentler western slope (Fig. ).作者: dysphagia 時(shí)間: 2025-3-26 06:11 作者: Irritate 時(shí)間: 2025-3-26 10:20
Fundamentals of Robotic Mechanical Systemsat its mouth in the southwest. The northern border of the Porcupine Seabight is difficult to define with no clear break of slope but a gradual transition from the Seabight to the Porcupine Bank and Celtic Shelf. With the borders as presented here, the Porcupine Seabight covers an area of 67,100 km. (Fig. 13.1).作者: neuron 時(shí)間: 2025-3-26 14:34 作者: Congregate 時(shí)間: 2025-3-26 18:08
Fundamentals of Rigid-Body Mechanics,such as cold-water coral carbonate mounds. Even though the mound features have a variety of origins, they all elevate from the seabed and protrude into the water column forming obstacles to bottom currents. Thus, they are often subject to erosion, providing hardgrounds and environmental conditions for organisms to settle and dwell.作者: 教義 時(shí)間: 2025-3-26 23:09 作者: 凝視 時(shí)間: 2025-3-27 03:21
Dynamics of Serial Robotic Manipulators, Spur was shaped during the opening of the Atlantic when a series of rift basins, partially separated by blocks of continental crust, were formed. Together, the Southwest Approaches and the Goban Spur cover 29,100 km. of the Irish seabed.作者: 序曲 時(shí)間: 2025-3-27 07:00
Special Topics in Rigid-Body Kinematics,ative shallow platform east of the margin is present where a thick sequence of sediment has infilled the northern Porcupine and Slyne Basins. This area has been the focus of intensive hydrocarbon exploration over the last few decades.作者: lavish 時(shí)間: 2025-3-27 11:29
An Overview of Robotic Mechanical Systems,0 m water depth in the south. The borders of the Rockall Trough with the Porcupine and Rockall Banks are clearly defined and can be identified by an abrupt increase in slope angle. Towards the north, these borders converge into a more gradually changing slope.作者: 牙齒 時(shí)間: 2025-3-27 16:04 作者: 貿(mào)易 時(shí)間: 2025-3-27 21:09
Iceberg Ploughmarksway or get dragged even further up the slope. The result is that icebergs leave marks in the soft sediments of the seafloor that usually follow gentle zigzag lines climbing up the slopes (Fig. 11.2–11.4).作者: 過(guò)渡時(shí)期 時(shí)間: 2025-3-27 22:11
Southwest Approaches and Goban Spur Spur was shaped during the opening of the Atlantic when a series of rift basins, partially separated by blocks of continental crust, were formed. Together, the Southwest Approaches and the Goban Spur cover 29,100 km. of the Irish seabed.作者: 職業(yè) 時(shí)間: 2025-3-28 02:18
Northernmost Irish Continental Marginative shallow platform east of the margin is present where a thick sequence of sediment has infilled the northern Porcupine and Slyne Basins. This area has been the focus of intensive hydrocarbon exploration over the last few decades.作者: 線 時(shí)間: 2025-3-28 07:06 作者: HEAVY 時(shí)間: 2025-3-28 13:39 作者: 拋射物 時(shí)間: 2025-3-28 18:09
An Overview of Robotic Mechanical Systems,ies of seawater as they remain relatively stable over time, only changing with the mixing of different water masses or with contact to the atmosphere. In addition to the conservative properties, numerous non-conservative properties are analysed like e.g. oxygen and carbon dioxide concentrations in the oceans.作者: somnambulism 時(shí)間: 2025-3-28 22:41
INSS Data Processingaining latitude, longitude and water depth (XYZ) coordinates, as digital elevation models (DEM) and raster data sets. For all geographic data presented in this atlas, the spatial reference datum is WGS1984 (Fig. 2.1).作者: indecipherable 時(shí)間: 2025-3-29 02:41
Above the Irish Seabedies of seawater as they remain relatively stable over time, only changing with the mixing of different water masses or with contact to the atmosphere. In addition to the conservative properties, numerous non-conservative properties are analysed like e.g. oxygen and carbon dioxide concentrations in the oceans.作者: 未開(kāi)化 時(shí)間: 2025-3-29 04:58 作者: Hallmark 時(shí)間: 2025-3-29 07:47 作者: capillaries 時(shí)間: 2025-3-29 15:18
Introduction attention and gets ignored. As Ireland’s deep-water seabed is hidden under several hundreds of metres of water, it has also historically received limited attention: what is out of sight is so often out of mind. This fundamentally changed when Ireland realised the scientific, as well as commercial, importance of its underwater realm.作者: GORGE 時(shí)間: 2025-3-29 16:32 作者: Stricture 時(shí)間: 2025-3-29 23:00 作者: Optometrist 時(shí)間: 2025-3-30 01:07 作者: Apogee 時(shí)間: 2025-3-30 06:47
An Overview of Robotic Mechanical Systems, attention and gets ignored. As Ireland’s deep-water seabed is hidden under several hundreds of metres of water, it has also historically received limited attention: what is out of sight is so often out of mind. This fundamentally changed when Ireland realised the scientific, as well as commercial, importance of its underwater realm.作者: Excise 時(shí)間: 2025-3-30 11:24 作者: BLANK 時(shí)間: 2025-3-30 16:08 作者: 藕床生厭倦 時(shí)間: 2025-3-30 19:24 作者: 為敵 時(shí)間: 2025-3-30 22:43 作者: mitten 時(shí)間: 2025-3-31 03:38
Fundamentals of Robotic Mechanical Systemseen 2000 and 2002 as part of the INSS. Data acquisition was carried out using a deep-water mutibeam echosounder system (Kongsberg-Simrad EM120) and two mid-water multibeam echosounder systems (Kongsberg-Simrad EM1002) on-board of the research vessels RV Bligh and RV Siren. After initial on board hyd作者: extinct 時(shí)間: 2025-3-31 07:58 作者: FRONT 時(shí)間: 2025-3-31 12:28
Geometry of General Serial Robots,that Pangea started to split apart creating a series of rift valleys. Eventually, this rifting split all the way through the continental crust and a new ocean basin was formed with two new smaller continents on either side: the North Atlantic, Europe and North America respectively. The gross morphol作者: 車(chē)床 時(shí)間: 2025-3-31 16:32 作者: 殖民地 時(shí)間: 2025-3-31 20:37 作者: OASIS 時(shí)間: 2025-4-1 00:06
Special Topics in Rigid-Body Kinematics,ed tens to several hundreds of metres deep into the continental margin. They often extend from the shelf break at 200 m water depth all the way down to the lower continental rise at approximately 2,500 m water depth funnelling large volumes of sediment and organic matter from shelf regions to the de作者: Cardiac 時(shí)間: 2025-4-1 04:13
Special Topics in Rigid-Body Kinematics,e (Fig. 8.1). The majority of seamounts are conically shaped when young but due to erosion become more irregularly shaped over time with circular to elliptic elongated bases and often flat summit areas. The slopes of seamounts can be quite steep, sometimes up to 60° (Fig. 8.2).作者: anesthesia 時(shí)間: 2025-4-1 09:13
