作者: 上腭 時(shí)間: 2025-3-21 20:47
978-90-481-4117-3Springer Science+Business Media Dordrecht 1992作者: GREG 時(shí)間: 2025-3-22 01:27 作者: 征稅 時(shí)間: 2025-3-22 06:25 作者: Inclement 時(shí)間: 2025-3-22 09:12
https://doi.org/10.1007/978-3-031-35003-0ifficult to detect in the field because the feeble surface expressions of the individual lineaments are commonly camouflaged by surface features such as linear sand dunes and yardangs. Their tectonic origin and rejuvenating nature are suggested by several indications: 1) their smooth passage across 作者: 叫喊 時(shí)間: 2025-3-22 15:01
https://doi.org/10.1007/978-3-031-35003-0 features in the U.S. and Canada. A . versus . graph of these features strongly resembles the similarly plotted curves of Lunar and Martian impact craters of the same size range, indicating that these large Earth features may have a similar origin and history. The one hundred-plus features mapped ar作者: 牙齒 時(shí)間: 2025-3-22 19:00
https://doi.org/10.1007/978-3-663-10291-5ment The craton core is now a horst of Archaean rocks. Minor structures indicate that gold mineralization along the fractures is syn- to post-rifting. Several remarkable features are associated with the fractures. These features are apparent in directions perpendicular to the trend of the fractures,作者: CLAIM 時(shí)間: 2025-3-22 21:22 作者: lesion 時(shí)間: 2025-3-23 04:26
https://doi.org/10.1057/9781137570505ction. Structural trends inferred from volcanological features display a dominantly north to north-westerly alignment within the province. Volcanic episodes date from late Tertiary (10 Ma) through to Recent, with the last eruption occurring approximately 190 years ago from the Kiejo eruptive..Compos作者: neoplasm 時(shí)間: 2025-3-23 06:04 作者: 平躺 時(shí)間: 2025-3-23 12:32 作者: CRUC 時(shí)間: 2025-3-23 13:55
Hegemony Versus Multilateralism,nic phase added material to the northwestern margin of the Guyanan craton. A suite of correlative rocks bounded by regional unconformities (herein referred to as a .) characterizes each period of deformation and amalgamation..The Guyana craton, consolidated during Archean events, is the structural u作者: 礦石 時(shí)間: 2025-3-23 21:44 作者: 贊成你 時(shí)間: 2025-3-23 23:22 作者: guzzle 時(shí)間: 2025-3-24 05:03 作者: CERE 時(shí)間: 2025-3-24 07:47
Dream of the Noble and the Beggarman of 12–13 km. It has a more complex history than some other interior basins because it is both a cratonic and a foreland basin. It shares a common origin with several North American Paleozoic basins in having formed over a preexisting rift zone. This rift zone — the Southern Oklahoma Aulacogen — was作者: FACET 時(shí)間: 2025-3-24 13:57 作者: enumaerate 時(shí)間: 2025-3-24 16:59 作者: Contend 時(shí)間: 2025-3-24 20:54 作者: Harpoon 時(shí)間: 2025-3-25 02:16 作者: 牽索 時(shí)間: 2025-3-25 06:11 作者: EXULT 時(shí)間: 2025-3-25 09:07
Basement Tectonics 7978-94-017-0833-3Series ISSN 0928-267X 作者: 直言不諱 時(shí)間: 2025-3-25 15:38
0928-267X Overview: 978-90-481-4117-3978-94-017-0833-3Series ISSN 0928-267X 作者: fatty-acids 時(shí)間: 2025-3-25 18:53
To Live the Things that I before Imaginedf the associated granitoids are of anatectic origin related to the thickening of a continental border. This border was created during a period of collision with a newly attached southern Gondwana continent, which now forms most of Patagonia, south of Tandilia.作者: Simulate 時(shí)間: 2025-3-25 22:06 作者: 純樸 時(shí)間: 2025-3-26 01:51
https://doi.org/10.1057/9781137570505tion into appropriate phase diagrams indicates that alkali basalts and basanites from the Sarabwe vent are transitional lavas of intermediate to low pressure evolution, with variable degrees of crustal contamination. Tephrite from the Fiteko vent shows signs of clinopyroxene + olivine fractionation at low pressure from more ‘primitive’ magma.作者: 存在主義 時(shí)間: 2025-3-26 07:26
Trotsky in the Prison Notebooks,n which imprinted a LS fabric on the Precambrian fabric. Existing basement rocks were dissected by Miocene leucogranite intrusions. During the D. phase the basement rocks were gravity nappes thrust southward. The basement reactivation is related to post-collision, continental convergence tectonics.作者: fixed-joint 時(shí)間: 2025-3-26 12:03 作者: 猜忌 時(shí)間: 2025-3-26 14:47 作者: inquisitive 時(shí)間: 2025-3-26 19:11
Tectonics of Some Spatial Arraysis suggested that global-scale linears (fold belts, volcanic chains, continental margins, oceanic ridges etc.) also have an underlying regularity and a tendency to polygonal patterns. The spacing in arrays is controlled by such factors as buckling, fracture mechanics, density and viscosity contrasts作者: CARE 時(shí)間: 2025-3-26 21:43
Counterclockwise Converging Basement Fracturing Patterns Across the Arabian Peninsula and Eastern Irifficult to detect in the field because the feeble surface expressions of the individual lineaments are commonly camouflaged by surface features such as linear sand dunes and yardangs. Their tectonic origin and rejuvenating nature are suggested by several indications: 1) their smooth passage across 作者: ligature 時(shí)間: 2025-3-27 03:45
Evidence of Large Horizontal Earth Movements features in the U.S. and Canada. A . versus . graph of these features strongly resembles the similarly plotted curves of Lunar and Martian impact craters of the same size range, indicating that these large Earth features may have a similar origin and history. The one hundred-plus features mapped ar作者: LASH 時(shí)間: 2025-3-27 08:48 作者: 傲慢人 時(shí)間: 2025-3-27 09:35 作者: incredulity 時(shí)間: 2025-3-27 16:53
Rift Related Magmatism and the Petrogenesis of Lavas from the Kiejo Eruptive, Rungwe Volcanic Provinction. Structural trends inferred from volcanological features display a dominantly north to north-westerly alignment within the province. Volcanic episodes date from late Tertiary (10 Ma) through to Recent, with the last eruption occurring approximately 190 years ago from the Kiejo eruptive..Compos作者: esculent 時(shí)間: 2025-3-27 21:29
Deformation and Intrusion in Deeply Buried Rocks: Creep, High-Angle Ductile and Brittle Shear, and Cractures and brittle-ductile or ductile shear zones that form at low or high angles (less than or more than 45°) to the axis of greatest compressive stress (σ.). A new Continuum criterion for deformation allows us to graph the stresses that result in flow (including creep), and virtually any orienta作者: GROUP 時(shí)間: 2025-3-28 01:01
Western Himalaya Basement Reactivationrtiary structures superimposed over the Precambrian fabric. The outer belt of epigra de metamorphics and granites comprising the Chail Unit was upthrust in a wedge shape along the steeply dipping Chail Thrust in the Western foothills. This thrust flattens eastward and gives rise to the south-vergent作者: BROW 時(shí)間: 2025-3-28 04:33 作者: 引水渠 時(shí)間: 2025-3-28 09:38 作者: 生意行為 時(shí)間: 2025-3-28 11:38 作者: Gullible 時(shí)間: 2025-3-28 18:30 作者: AWRY 時(shí)間: 2025-3-28 19:32 作者: tenosynovitis 時(shí)間: 2025-3-28 23:15
Fundamental Crustal Lineaments and Transverse Structural Zones in Continental Riftsoften intense fracturing, along trends which are generally transverse or oblique to the main rift-bounding structures. The transverse zones often delimit major re-orientations in the rift trend, or link paired offset margins, and are foci for magmatic activity and heat flow anomalies. Furthermore, t作者: 思想上升 時(shí)間: 2025-3-29 06:21 作者: crucial 時(shí)間: 2025-3-29 07:44
Basement Extension on the Newfoundland Continental Margin (Canadian East Coast)ridges and a complex continent-ocean transition zone formed during several Mesozoic rifting periods. Recent industry seismic lines and several deep seismic reflection profiles (Lithoprobe East) allow for the recognition of coherent reflections of intra-basement provenance..Precambrian and early Pale作者: Decrepit 時(shí)間: 2025-3-29 12:54
Structural Fabric of the North American Continent, as Defined by Gravity Trendsends is demonstrated by the close correspondence between gravity domains defined on the basis of trend patterns, and structural domains based primarily on geological criteria. This relationship provides a powerful tool for investigating Precambrian basement geology in platform-covered regions of the作者: 單片眼鏡 時(shí)間: 2025-3-29 19:31 作者: 嚴(yán)厲譴責(zé) 時(shí)間: 2025-3-29 21:39
Tectonics of Some Spatial Arraysemarkably coincident with inflections in the seismic profile. It is suggested that fault spacing is dependent on the upper brittle part of the crust..Archean plutons occur in wider-spaced arrays (65 km to 90 km), and with either convection or buoyant-layer models, this spacing indicates a magma sour作者: CRUC 時(shí)間: 2025-3-30 01:33 作者: chondromalacia 時(shí)間: 2025-3-30 04:12 作者: Mutter 時(shí)間: 2025-3-30 10:12 作者: 瘋狂 時(shí)間: 2025-3-30 15:13 作者: cinder 時(shí)間: 2025-3-30 19:27 作者: 暴發(fā)戶(hù) 時(shí)間: 2025-3-30 21:51
Tectonic Evolution of Northwestern South America “rift and drift” phases of the breakup of Pangea. During latest Cretaceous and into the Paleocene, microplate collision affected the entire South American margin, locally forming a suture. Interactions with the Caribbean and Nazca plates intensified and, starting in Miocene time with a Pliocene pea作者: Urea508 時(shí)間: 2025-3-31 01:23 作者: Ambiguous 時(shí)間: 2025-3-31 07:43 作者: prostatitis 時(shí)間: 2025-3-31 12:54 作者: 小步舞 時(shí)間: 2025-3-31 14:55
Fundamental Crustal Lineaments and Transverse Structural Zones in Continental Rifts as kinematic analogues of oceanic transform faults. However, detailed seismic interpretation and structural mapping of transverse zones in the North Sea Rift have revealed a connection between the transverse zones and fundamental basement lineaments in N.W. Europe. Major offsets of the Mesozoic Nor作者: 高貴領(lǐng)導(dǎo) 時(shí)間: 2025-3-31 19:44
Tectonic Controls on the Lake Victoria Basinund the craton margins, and intersection among a series of NW-trending strike-slip faults which transect the craton. Casual observation might suggest that the basin was formed by meteorite impact (Saul and Glaholm, 1981), but there is no geologic evidence (i.e., impact breccias, tektites, radial fra作者: 最高點(diǎn) 時(shí)間: 2025-3-31 22:13
Basement Extension on the Newfoundland Continental Margin (Canadian East Coast)ower crustal zone and underlies most of the Newfoundland offshore structural elements. A linked system of synthetic and antithetic faults associated with this crustal detachment now borders the structural units of the shelf..The widespread reactivation of pre-existing Precambrian and Paleozoic zones作者: 佛刊 時(shí)間: 2025-4-1 04:12 作者: Osteoarthritis 時(shí)間: 2025-4-1 06:11
Neotectonic Framework of the United Statesuthern Appalachian highlands, the Arkansas-St. Lawrence lowland and the Mid-Continent Arch. The north-trending extensional faults appear related to right-lateral strike slip along the north west-trending zones. They are most prominent in the Great Basin in the west, but are also present in the east,作者: mastopexy 時(shí)間: 2025-4-1 13:53
The Karakoram Crustal Fracture: Oblique Convergence in the Asiatic Tethys作者: 短程旅游 時(shí)間: 2025-4-1 17:02 作者: jaundiced 時(shí)間: 2025-4-1 20:24 作者: LAP 時(shí)間: 2025-4-2 00:45
