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201.
Limited modification of mid-latitude landscapes by ice sheets: The case of northeast Scotland 总被引:1,自引:0,他引:1
The paper uses a case study in Scotland to examine the amount and processes of landscape modification by Quaternary ice sheets. There is an inverse correlation between the distribution of landforms of glacial erosion and pre-glacial landscape remnants in northeast Scotland. The implication is that in places ice sheets can preserve a pre-glacial landscape unscathed, while elsewhere they remove the pre-glacial weathered rock. The location of glacial protection or erosion is strongly influenced by the topography and its influence on former ice sheet flow and basal thermal regime. The classic glacially eroded landscape of areal scouring can be produced by the removal of only 10–50 m of weathered rock. Furthermore rock basins, often regarded as the hallmark of glacial erosion, may be directly inherited from the pre-glacial pattern of deep weathering. 相似文献
202.
203.
Significance of MORB-derived Amphibolites from the Aracena Metamorphic Belt, Southwest Spain 总被引:2,自引:0,他引:2
CASTRO ANTONIO; FERNANDEZ CARLOS; DE LA ROSA JESUS D.; MORENO-VENTAS IAKI; ROGERS GRAEME 《Journal of Petrology》1996,37(2):235-260
The Aracena metamorphic belt, in the southwest Iberian Massif,is characterized by the presence of MORB-derived amphibolitesand continental rocks deformed and metamorphosed during theHercynian orogeny. Geochemical relationships of these amphibolitesindicate the existence of a multiple fractionation process froma set of parental magmas, implying the existence of a multi-chambersystem beneath the ridge where the basalt protolith was extruded.Neodymium isotopic ratios are typical of MORB, and oxygen isotopesindicate that these amphibolites have been derived from theuppermost part of the oceanic crust. Thermal evolution, revealedfrom the study of chemical variations in the amphibole chemistry,is interpreted as resulting from subduction in a low-pressureregime in which the thermal structure of the continental hanging-wallplayed an important role. This continental wall was previouslyheated by subduction of a slab window resulting from migrationof a triple junction along the continental edge during plateconvergence. Three petrologic arguments support this tectonicmodel. These are: (1) the low-pressure inverted metamorphicgradient of amphibolites of the oceanic domain; (2) the high-temperature-low-pressure metamorphism of the continental hanging wall; (3)the early intrusion of boninites into the continental domain.
*Corresponding author. 相似文献
204.
Studyonthefeatureselectionandclassifica┐tionefectofprecursorydataofgroundtiltZHENG-YUANLI(李正媛),DE-FUCHEN(陈德福),YI-LINWU(吴奕麟)a... 相似文献
205.
CharacteristicsoffaultrocksandpaleoearthquakesourcealongtheKoktokayErtaifaultzone,Xinjiang,ChinaLANBINSHI1)(史兰斌)CHUANYON... 相似文献
206.
LinTRODUCTIONANDAIMSTheaimsofthisStUdyaretointroducenewtechniquesforanalysingfloodflowsfromsedimentarrangementmsapproachincorporatestheeffectsofflotvonthedevelopmentofrouglmessontheriverbed,andnot,asismostlythecase,theeffectsofbedroughnessonflow.Differentacsofflows,includingthemaalmumfloodflowarereconsmictedfromfloworientahonsofparticlesoveranentiregravCIbar.DuetOtheddricultiesinvolvedinobtaininglargeparticlesamples,studiesonpAncleOrientationsintheliteratUrearerare.WhilstmoStanalyse… 相似文献
207.
Akindofinformationonshorttermandimminentearthquakeprecursors—researchonatmosphericelectricfieldanomaliesbeforeearthquakesJI... 相似文献
208.
On the crystallinity of illite in diagenesis and anchimetamorphism A simple method to estimate the degree of “crystallinity” of illite has been used for several years in three French laboratories. Many results, which are unpublished, were obtained; three examples are presented in this paper. They show the sensibility of the method, which allows one to appreciate, above all other methods, burial diagenesis, the front of metamorphism, or some regional areas of very weak metamorphism. 相似文献
209.
P.TEILHARD DE CHARDIN 《地质学报》1937,(Z1)
Over a continental area, the sediments are mostly found, either asoriginally spread by water along the slopes (gravels or loams: fan-deposits), or as accumulated by streams in the bottom of the basins(lake-deposits, or fluvial plains), either as disseminated by wind (sand-dunes and loess deposits). 相似文献
210.
P.TEILHARD DE CHARDIN 《地质学报》1926,5(3)
During the summer of 1923, we were so lucky F. Licent and myself as to get, in three different places, the first records of the palaeolithic Man in China. 相似文献