標(biāo)題: Titlebook: Geology of Holocene Barrier Island Systems; Richard A. Davis Book 1994 Springer-Verlag Berlin Heidelberg 1994 Barrier Islands.Coast.Coasta [打印本頁(yè)] 作者: 連結(jié) 時(shí)間: 2025-3-21 17:46
書目名稱Geology of Holocene Barrier Island Systems影響因子(影響力)
書目名稱Geology of Holocene Barrier Island Systems影響因子(影響力)學(xué)科排名
書目名稱Geology of Holocene Barrier Island Systems網(wǎng)絡(luò)公開度
書目名稱Geology of Holocene Barrier Island Systems網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Geology of Holocene Barrier Island Systems被引頻次
書目名稱Geology of Holocene Barrier Island Systems被引頻次學(xué)科排名
書目名稱Geology of Holocene Barrier Island Systems年度引用
書目名稱Geology of Holocene Barrier Island Systems年度引用學(xué)科排名
書目名稱Geology of Holocene Barrier Island Systems讀者反饋
書目名稱Geology of Holocene Barrier Island Systems讀者反饋學(xué)科排名
作者: Postulate 時(shí)間: 2025-3-21 21:35
Digital Design from the VLSI Perspectivehis condition combined with the broad range in tidal prism and the human influence have produced a unique coastal complex. Another important aspect of this coast is the rapid change which commonly takes place under such pronounced low-energy conditions.作者: FUME 時(shí)間: 2025-3-22 04:09 作者: WAG 時(shí)間: 2025-3-22 05:23
Barriers of the Florida Gulf Peninsula,his condition combined with the broad range in tidal prism and the human influence have produced a unique coastal complex. Another important aspect of this coast is the rapid change which commonly takes place under such pronounced low-energy conditions.作者: Interregnum 時(shí)間: 2025-3-22 09:46 作者: 牛馬之尿 時(shí)間: 2025-3-22 14:58
Book 1994unes, washover fans, marshes, tidal flats, estuaries, lagoons, and tidal inlets. The morphodynamics of these fragile coastal systems provide a further complication to this coastal type. Although barrier islands comprise only 15% of the world‘s coastline, they have received a far greater proportion o作者: 牛馬之尿 時(shí)間: 2025-3-22 18:35
,Barrier Island Systems — a Geologic Overview,me that do not. It is further complicated by such variables a sea level change, sediment supply and the relative influence of wave- and tide-dominated processes..Fortunately, there is also a great deal of predictability to barrier island geology and stratigraphy. The nature and relative positions of作者: malign 時(shí)間: 2025-3-22 23:28
The Outer Banks of North Carolina, microtidal (0.9 m tidal range) high wave energy (1.7m average wave height) hydrographic setting. Holocene sedimentation and coastal evolution have been a function of five major depositional processes: (1) eustatic sea-level rise and barrier-shoreline transgression; (2) lateral tidal inlet migration作者: 敲竹杠 時(shí)間: 2025-3-23 02:52
Texas Barriers,a dominant westerly flow in the northern Gulf of Mexico (LeBlanc and Hodgson 1959). This westerly flow and the regional distribution of barrier islands led some early workers to conclude that Texas barrier islands were deposited by littoral drift reworked from the Mississippi River. More recent geol作者: 細(xì)胞膜 時(shí)間: 2025-3-23 08:13 作者: Oscillate 時(shí)間: 2025-3-23 10:42
Barriers of the Florida Gulf Peninsula,marsh system and an open coast mangrove system. The entire barrier system has developed during the past 3000 years. This coastal barrier complex is the most morphologically diverse continuous barrier island system in the world. The complete spectrum of barrier island and tidal inlet morphologies is 作者: faultfinder 時(shí)間: 2025-3-23 16:27
New Jersey and Delmarva Barrier Islands,e New Jersey and Delmarva Peninsula, the wave-dominated barrier islands occur immediately south of the main interfluve headlands of the respective peninsulas. The tide-dominated barriers occur downdrift, and south of the wave-dominated barriers..The barriers in wave-dominated sections of the New Jer作者: 自負(fù)的人 時(shí)間: 2025-3-23 18:38 作者: Bmd955 時(shí)間: 2025-3-23 22:44
New England Barriers,Gulf of Mexico shoreline. Several episodes of glaciation have left New England with a rocky, irregular shoreline that reflects the bedrock fabric of the region and the results of differential weathering. Glaciation is also responsible for the highly varied and often isolated sediment sources (Cape C作者: 尖 時(shí)間: 2025-3-24 03:34 作者: 匍匐 時(shí)間: 2025-3-24 09:46
https://doi.org/10.1007/978-981-16-5955-3n landward migration of both barrier limbs of the cuspate foreland. A decline in the rate of sea-level rise since 4000 b.p. resulted in relative shoreline stabilization and deposition of contrasting coastal sedimentary sequences. The higher-energy, north and northeast barrier limbs (Core-Portsmouth 作者: Pageant 時(shí)間: 2025-3-24 10:57 作者: textile 時(shí)間: 2025-3-24 18:30
Yojana Sharma,Parnika Shrivastava,Mohit Pant They also show that tectonic activity is a minor factor in determining barrier type or size bacause the Tijuana River-Silver Strand barrier system is in a tectonically stable area and the Eel River-Humboldt Bay system is in a tectonically active one. The Tijuana and Eel Rivers both deliver large am作者: 薄荷醇 時(shí)間: 2025-3-24 20:56
,Unseren t?glichen Chat gib uns heute,deposits over a comparatively large lagoon area. In wide barrier lagoons, inletjet fields are small with respect to the large surface areas of the lagoon and repletion is limited. Fine-grained sediments are primarily stirred by wave currents and distributed over shallow lagoonal bays. Resettling of 作者: PRO 時(shí)間: 2025-3-24 23:32 作者: Postulate 時(shí)間: 2025-3-25 05:10
Alina Hruba,Maria Claudia Solarte Vasquezampening within these basins have produced macro-tidal to microtidal conditions that have been subject to change over time. The large bays and sounds, the indented nature, and the multitude of shoreline orientations of the New England coast cause a wide range in wave-energy conditions. Thus, the hyd作者: homeostasis 時(shí)間: 2025-3-25 10:14
Digital Dilemmas in Organizations,mstick configurations in response to the upper mesotidal range and large, obliquely approaching (from SE) waves in the area. The barrier islands were uplifted 2.5–3.0 m during the Good Friday earthquake of 1964. The shoreline of the islands pro-graded at the rate of 60m/year in the decade that follo作者: ULCER 時(shí)間: 2025-3-25 15:19 作者: COM 時(shí)間: 2025-3-25 17:21 作者: 不開心 時(shí)間: 2025-3-25 22:28 作者: BIAS 時(shí)間: 2025-3-26 01:46 作者: hyperuricemia 時(shí)間: 2025-3-26 04:59 作者: 身體萌芽 時(shí)間: 2025-3-26 10:10 作者: Gentry 時(shí)間: 2025-3-26 13:48 作者: 向外供接觸 時(shí)間: 2025-3-26 20:15 作者: 鎮(zhèn)壓 時(shí)間: 2025-3-26 22:47 作者: 故意 時(shí)間: 2025-3-27 03:36 作者: 歌唱隊(duì) 時(shí)間: 2025-3-27 05:39
https://doi.org/10.1007/978-3-642-78360-9Barrier Islands; Coast; Coastal Geology; Küstengeologie; Sediment; Sedimentologie; Stratigraphie; Stratigra作者: sed-rate 時(shí)間: 2025-3-27 13:29
Digital Systems in Oral Pathologyme that do not. It is further complicated by such variables a sea level change, sediment supply and the relative influence of wave- and tide-dominated processes..Fortunately, there is also a great deal of predictability to barrier island geology and stratigraphy. The nature and relative positions of作者: 軍械庫(kù) 時(shí)間: 2025-3-27 16:47
https://doi.org/10.1007/978-981-16-5955-3 microtidal (0.9 m tidal range) high wave energy (1.7m average wave height) hydrographic setting. Holocene sedimentation and coastal evolution have been a function of five major depositional processes: (1) eustatic sea-level rise and barrier-shoreline transgression; (2) lateral tidal inlet migration作者: 流動(dòng)性 時(shí)間: 2025-3-27 18:38
https://doi.org/10.1007/b117975a dominant westerly flow in the northern Gulf of Mexico (LeBlanc and Hodgson 1959). This westerly flow and the regional distribution of barrier islands led some early workers to conclude that Texas barrier islands were deposited by littoral drift reworked from the Mississippi River. More recent geol作者: Spartan 時(shí)間: 2025-3-27 22:18 作者: phlegm 時(shí)間: 2025-3-28 03:19
Digital Design from the VLSI Perspectivemarsh system and an open coast mangrove system. The entire barrier system has developed during the past 3000 years. This coastal barrier complex is the most morphologically diverse continuous barrier island system in the world. The complete spectrum of barrier island and tidal inlet morphologies is 作者: 深淵 時(shí)間: 2025-3-28 06:17 作者: Circumscribe 時(shí)間: 2025-3-28 11:22 作者: magnanimity 時(shí)間: 2025-3-28 15:21
Alina Hruba,Maria Claudia Solarte VasquezGulf of Mexico shoreline. Several episodes of glaciation have left New England with a rocky, irregular shoreline that reflects the bedrock fabric of the region and the results of differential weathering. Glaciation is also responsible for the highly varied and often isolated sediment sources (Cape C作者: Onerous 時(shí)間: 2025-3-28 21:23
Digital Dilemmas in Organizations,of south-central Alaska. Three of the compartments contain multiple beach ridges that form beach-ridge plains several km wide in places, and one is a series of prograding, delta-front barrier islands. This anamolous occurrence of a major depositional coastline in such a tectonic setting is the resul作者: HEPA-filter 時(shí)間: 2025-3-29 01:36
Law and Philosophy Libraryhttp://image.papertrans.cn/s/image/864597.jpg作者: 大廳 時(shí)間: 2025-3-29 05:14
2509-310X the text, drawn from a wide range of sources including the extensive collection held by the CSIRO Radio Astronomy Image Archive. The book will be an essential reference for readers interested in the scientific978-3-319-91843-3Series ISSN 2509-310X Series E-ISSN 2509-3118
