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91.
92.
大别山北部红刚玉矿产在太古代大别山群黑云角门外长片麻岩以及超基性岩中。赋存红刚玉的刚玉黑云二长片麻岩的原始岩石为富铝泥质岩,在角门岩相变质条件下,通过两种脱硅方式,即变质分异作用和超基性岩侵位,形成刚玉黑云二长片麻岩。它们形成的温压条件:T=500℃~700℃,P=0.4~0.7GPa。刚玉形成的可能的化学机制是白云母在缺硅条件下的分解。 相似文献
93.
Tree stem (>2 m tall) mortality was assessed following a late dry‐season wildfire across a seasonally flooded elevation gradient at Workshop Jungle, near Darwin, in the Northern Territory of Australia. For all species combined, dead stems had significantly smaller diameter at breast height (dbh) than living stems. Assessment of tree‐stem damage following a tropical cyclone at Cobourg Peninsula, NT, revealed that damaged stems had significantly greater dbh than undamaged stems for all tree species sampled across a boundary between monsoon rainforest and savanna. A greater proportion of stems were damaged by the cyclone than by the fire (28 per cent as against 18 per cent), although there were considerable between‐community differences in the proportion of damaged stems at the two sites. The fire caused little impact (<10 per cent) on total basal area of three different forest communities on the elevation gradient at Workshop Jungle. The cyclone was found to cause >50 per cent damage to total basal area of three different communities on Cobourg Peninsula. It is suggested that the combination of a cyclone followed by an intense fire in storm debris could potentially destroy a monsoon rainforest through its impact on all tree‐size classes. This may explain why some monsoon rainforests rapidly contracted following Cyclone Tracy that destroyed the city of Darwin on Christmas Day, 1974. 相似文献
94.
吉林省北部A型花岗岩的初步认识 总被引:2,自引:0,他引:2
分布在吉林省北部的香水、治安一带的正长花岗岩、碱长花岗岩,研究后认为属A型花岗岩。其行征钾长石为微斜长石一条纹长石,斜长石大部分为奥长石An=13-17。并有碱性碱物无辉石。 相似文献
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Rock salt is approximately 1000 times more soluble than limestone and thus displays high rates of geomorphic evolution. Cave stream channel profiles and downcutting rates were studied in the Mount Sedom salt diapir, Dead Sea rift valley, Israel. Although the area is very arid (mean annual rainfall ≈ 50 mm), the diapir contains extensive karst systems of Holocene age. In the standard cave profile a vertical shaft at the upstream end diverts water from a surface channel in anhydrite or clastic cap rocks into the subsurface route in the salt. Mass balance calculations in a sample cave passage yielded downcutting rates of 0–2 mm s?1 during peak flood conditions, or about eight orders of magnitude higher than reported rates in any limestone cave streams. However, in the arid climate of Mount Sedom floods have a low recurrence interval with the consequence that long-term mean downcutting rates are lower: an average rate of 8·8 mm a?1 was measured for the period 1986–1991 in the same sample passage. Quite independently, long-term mean rates of 6·2mm a?1 are deduced from 14C ages of driftwood found in upper levels of 12 cave passages. These are at least three orders of magnitude higher than rates established for limestone caves. Salt cave passages develop in two main stages: (1) an early stage characterized by high downcutting rates into the rock salt bed, and steep passage gradients; (2) a mature stage characterized by lower downcutting rates, with establishment of a subhorizontal stream bed armoured with alluvial detritus. In this mature stage downcutting rates are controlled by the uplift rate of the Mount Sedom diapir and changes of the level of the Dead Sea. Passages may also aggrade. These fast-developing salt stream channels may serve as full-scale models for slower developing systems such as limestone canyons. 相似文献
98.
Gregory N. Tsokas 《Pure and Applied Geophysics》1995,144(1):117-134
The anomalies which are shown on the gravity and aeromagnetic data of the Chalkidhiki peninsula of Northern Greece reveal
the presence of three concealed dense and magnetized bodies. The ophiolitic belt which continues northwards of the geophysical
anomalies suggests that they are caused by structures which belong to it.
Multiple source Werner deconvolution shows that the lower surfaces of buried bodies in Toroneos Gulf and the one onshore are
concave upwards.
The northern concealed body has a width of 16 kilometers, while the southern one is 8 kilometres in width. A three-dimensional
model, well constrained, gives an estimate of the dimensions of the onshore feature.
The edges of the bodies, delineated by the terracing method, are formed by faults along the trend of the Hellenides orogenic
belt. The edges of the body in the outer part of Toroneos Gulf may be associated with seismic swarms that occurred in the
1980s. 相似文献
99.
北半球阻塞高压的维持Ⅱ:瞬变扰动强迫和平均流位涡平流的形成 总被引:4,自引:2,他引:4
着重探讨大西洋阻高和东亚阻高个例中瞬变扰动位涡(涡度)输送强迫和太平洋阻高中平均流位涡平流的形成机理。结果表明,扰动在阻高西南部西风分流区因形变而产生的扰动拟能向更小尺度串级过程,并不是扰动位涡输送强迫形成的必要机理。扰-流相互作用在阻高西(北)部非分流气流中也十分显著。数值试验表明,这一相互作用也可能是扰动强迫作用形成的机理。而青藏高原和附近海陆对比的强迫作用则可能是太平洋阻高中平均流的位涡平流形成的重要因素。对比分析表明,阻高维持机制的地域性差别可能与其上游(如青藏高原地区、落基山脉)地形和热源强迫作用不同有关。 相似文献
100.
New finds of siliceous microfossils, mainly diatoms, are reported from hard limestone levels in the Campanian cherty Mishash Formation, Negev, Israel. Twenty taxa were recognized, of which Melosira campaniensis and Trinacria negeviensis are new species. Representatives of Ebridians are reported for the first time from Cretaceous sediments. Calcareous nannofossils are usually few and poorly preserved. The diversity of the micro- and nannofossil assemblages vary through the succession and points to fluctuations in the palaeoenvironmental conditions from restricted to more normal marine. The moderate preservation of the opaline microfossils within the limestones is probably the result of early diagenetic lithification. 相似文献