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571.
热林复式花岗岩体,总体为从边部到中部由细粒似斑状二长花岗岩、中粒似斑状二长花岗岩和边部补充期花岗斑岩5个侵入体组成的燕山期同源岩浆结构演化系列.属钙碱性系列,弱过铝质的Ⅰ型向S型过渡特征.成矿类型为蚀变花岗岩、石英脉型和角岩型3种,并划分为黄铁矿±黄铜矿—石英脉,黄铁矿—黄铜矿±辉钼矿—石英脉,辉钼矿±黄铜矿—石英脉及黄铜矿—石英—方解石脉4个成矿作用阶段. 相似文献
572.
573.
黄连沟钽、铌、铍矿产于燕山晚期花岗伟晶岩脉中,伟晶岩脉即为矿体、矿化体,该矿为明显的稀有金属伟晶岩脉矿床.矿区花岗伟晶岩脉众多,成群出现,单个脉体规模较大,加之铌、钽重砂异常明显,这些不仅显示了本区有很好的找矿前景,同时为今后的勘查提供了直接的找矿标志. 相似文献
574.
Bathymetric and sub-bottom acoustic data were collected in Laguna San Rafael, Chile, to determine sediment yields during the Little Ice Age advance and subsequent retreat of San Rafael Glacier. The sediment volumes and subaqueous landforms imaged are used to interpret the proglacial dynamics and estimate erosion rates from a temperate tidewater glacier over a complete advance-retreat cycle. Sediment yields from San Rafael Glacier averaged 2.7 × 107 m3/a since the end of the Little Ice Age, circa AD 1898, corresponding to average basin-wide erosion rates of 23 ± 9 mm/a; the highest erosion rates, 68 ± 23 mm/a, occurred at the start of the retreat phase, and have since been steadily decreasing. Erosion rates were much lower during glacial advance, averaging at most 7 mm/a, than during retreat. Such large glacial sediment yields over two centuries of advance and retreat suggest that the contribution of sediments stored subglacially cannot account for much of the sediment being delivered to the terminus today. The detailed sub-bottom information of a proglacial lagoon yields important clues as to the timing of erosion, deposition and transfer of glacigenic sediments from orogens to the continental shelves, and the influence of glacier dynamics on this process. 相似文献
575.
Little Ice Age (LIA) fluctuations of Glaciar Río Manso, north Patagonian Andes, Argentina are studied using information from previous work and dendrogeomorphological analyses of living and subfossil wood. The most extensive LIA expansion occurred between the late 1700s and the 1830-1840s. Except for a massive older frontal moraine system apparently predating ca. 2240 14C yr BP and a small section of a south lateral moraine ridge that is at least 300 yr old, the early nineteenth century advance overrode surficial evidence of any earlier LIA glacier events. Over the past 150 yr the gently sloping, heavily debris-covered lower glacier tongue has thinned significantly, but several short periods of readvance or stasis have been identified and tree-ring dated to the mid-1870s, 1890s, 1900s, 1920s, 1950s, and the mid-1970s. Ice mass loss has increased in recent years due to calving into a rapidly growing proglacial lake. The neighboring debris-free and land-based Glaciar Frías has also retreated markedly in recent years but shows substantial differences in the timing of the peak LIA advance (early 1600s). This indicates that site-specific factors can have a significant impact on the resulting glacier records and should thus be considered carefully in the development and assessment of regional glacier chronologies. 相似文献
576.
577.
578.
与加仁岩体有关的铜多金属矿床(点)较多,岩体构造复杂。在岩体分布区,划分岩体内部和外部宏观构造,查明不同构造之间的区别和联系,应是找矿的前题和基础,更是评价和预测矿产资源潜力的必要条件和首要任务。 相似文献
579.
The reconstruction of the climatic history during the past several hundred years requires a sufficient geographical coverage
of combined climate proxy series. Especially in order to identify causal connections between the atmosphere and the ocean,
inclusion of marine records into composite climate time series is of fundamental importance. We present two skeletal δ
18O chronologies of coral skeletons of Diploria labyrinthiformis from Bermuda fore-reef sites covering periods in the nineteenth and twentieth centuries and compare them with instrumental
temperature data. Both time series are demonstrated to display sea-surface temperature (SST) variability on inter-annual to
decadal time scales. On the basis of a specific modern δ
18O vs instrumental SST calibration we reconstruct a time series of SST anomalies between AD 1350 and 1630 covering periods
during the Little Ice Age. The application of the coral δ
18O vs temperature relationship leads to estimates of past SST variability which are comparable to the magnitude of modern variations.
Parallel to δ
18O chronologies we present time series of skeletal bulk density. Coral δ
18O and skeletal density reveal a strong similarity during Little Ice Age, confirming the reliability of both proxy climate
indicators. The past coral records, presented in this study, share features with a previously published climate proxy record
from Bermuda and a composite time series of reconstructed Northern Hemisphere summer temperatures. The coral proxy data presented
here represent a valuable contribution to elucidate northern Atlantic subtropical climate variation during the past several
centuries.
Received: 9 November 1998 / Accepted: 13 September 1999 相似文献
580.
ABSTRACT. Even the casual visitor cannot fail to notice unusual activity on the slopes of Northern California's Mount Shasta. Prayer flags, altars, and crystals are found in the meadows; drumming, chanting, and meditation are commonplace. Non‐indigenous spiritual pilgrims have found Mount Shasta a sacred place. An amorphous group of spiritual seekers, these are sometimes referred to as “New Age” adherents or “Crystal People.” Within the Shasta‐Trinity National Forest, the situation of this sacred site exemplifies the difficulties of reconciling nonsecular claims to public lands with secular management mandates. Spiritual activism at Mount Shasta includes recently successful opposition to development of a Forest Service‐endorsed ski area. Using a questionnaire survey and interviews, we compare the characteristics, activities, and attitudes toward resource management of spiritual pilgrims and others who visit Mount Shasta's meadows. Conclusions are drawn about the environmental values and concerns of all visitors and of spiritual pilgrims in particular, including some that bear on pilgrim activities and ecological restoration efforts. 相似文献