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11.
湘西南采金“信”的地质解释 总被引:2,自引:0,他引:2
在湘西南民间开采脉金的活动中,人们积累了很多识别金富集的标志,简称“信”。本文收集列举了25种“信”,并相应地作了地质解释,评估了含金情况。从金的地球化学特性,论述了“信”与金富集的内在联系。 相似文献
12.
The West Kunlun orogenic belt is located at the conjunction of the paleo-Asian tectonic system and the Tethys tectonic system.
Petrological and mineralogical studies of the Early Cambrian metamorphic surface crust in this region have shown that in case
the metamorphism reached low-temperature granulate facies, the typical mineral assemblage is biotite-garnet-silimanite-K feldspar-plagioclase-quartz.
The peak metamorphic temperatures are within the range of 720–740°C and the pressure is 0.6 GPa ±. Three types of metamorphic
zircon have been detected in the metamorphic rocks: the complex inclusion-bearing type ; the early relic zircon inclusion-bearing
type; and the inclusion-free type. SHRIMP age determination of these three types of metamorphic zircon have revealed that
these zircons were formed principally during 400–460 Ma, indicating that pre-Cambrian metamorphic surface crust rocks underwent
low-temperature granulite facies metamorphism during the Caledonian. In combination with the geological characteristics of
this region, it is considered that when the oceanic basin was closed, there occurred intense intracontinental subduction (type
A), bringing part of the Early Cambrian metamorphic basement in this region downwards to the lower crust. Meanwhile, there
were accompanied with tectonic deformation at deep levels and medium- to high-grade metamorphism. This study provided important
chronological and mineralogical evidence for the exploration of the evolutionary mechanism and process of the West Kunlun
Early Paleozoic.
Part of the results from the research project “ Research on the West Kunlun pre-Cambrian tectonic events” under the program
“ Research on the important geological problems of China’ s pre-Cambrian” (No. 200113900070) sponsored by the China National
Geological Surveying Bureau. 相似文献
13.
通过对郑州望京楼遗址出土的二里头文化时期石杵和石臼进行淀粉粒分析,发现了5类可鉴定的不同形态淀粉粒,主要为粟黍类、小麦族(Triticeae)、薏苡属(Coix)、栎属(Quercus)和豆科(Fabaceae)等,以及部分未知种属的淀粉粒。石臼和石杵的使用部位形态多样的淀粉粒表明此类工具在当时被用于加工处理多种植物种子或果实。望京楼遗址二里头文化时期石器上粟、黍以及小麦等多种农作物淀粉粒的发现,同时结合二里头、南洼、皂角树等二里头文化遗址植物浮选结果,表明二里头文化时期中原腹心地区已普遍存在多品种的农作物种植。 相似文献
14.
Zhao Kang Zhou Yun Yu Xiang Yan Yajing Song Yufeng Wang Junqiang Suo Tianyuan Guo Xiao 《Natural Resources Research》2021,30(5):3839-3852
Natural Resources Research - Depletion of shallow mineral resources caused by deep mining has become an inevitable trend, and deep mining can increase safety accidents and geological hazards.... 相似文献
15.
Zhao Baoren 《中国海洋湖沼学报》1986,4(2):159-170
Since Simpson and Hunter proposed in 1971 the idea that shallow water fronts were induced by tidal mixing, many authors have
investigated the tide induced shallow water fronts in various areas. It was generally assumed that a critical value of the
stratified parameterK=log10(H/U
3) may be used to identify the location of these fronts. Here, H means the depth of sea waler. U denotes the characteristic
velocity of tidal current. and the critical value ofK is generally laken as 1.8–2.0.
In this paper. Simpson-Hunter’s stratified parameterK was calculated by using quasi-maximum current velocity (which consists of the six main tidal constituents. i.e.M
2.S
2,O
1.K
1.M
4,MS4) in the H ranghai Sea (Yellow Sea) and in the northern Donghai Sea (East China Sea) as well. Caleulated results show that
the areas of the Subei (the northern part of Jiangsu) Shoal. the area off the mouth area of the Changjiang (the Yangtze) River,
along the coast of Shandong Peninsula. and along the western coast of Korea, the tidal mixing is strong. Calculations also
show that along the whole boundary of the HCWM and also along the western boundary of the cyclonic eddy in the northern Donghai
Sea, i.e. along the fronts, the value ofK is found to be very close to the eritical value 1.8. It is also to be noied that at these locations, the temperature of the
surface water is very low. These clearly show that shallow water fronts in the Huanghai Sea and in the northern Donghai Sea
as well, are induced by tidal mixing.
Contribution No. 1241 from Institute of Oceanology, Academia Sinica.
This paper was published in Chinese in theOcean. et Limn. Sinica
16(6): 451–459, 1985. 相似文献
16.
川藏公路中段地质灾害现象的航空遥感研究 总被引:2,自引:0,他引:2
川藏公路巴塘至林芝段位于我国青藏高原东南部,该地区是现今地壳运动十分强烈的地区之一,地形起伏强烈,气候变化多样,因此地质灾害十分发育,川藏公路就穿过这样一个复杂的地区。为查明公路沿线的地质灾害分布情况,90年代初,地矿部航空物探遥感中心沿川藏公路进行了彩色红外航空摄影,比例尺为1∶6万。通过彩色红外航片的解译及野外实地观测,圈定出滑坡、泥石流及崩塌等灾害现象,并对这些灾害的强度、活动性及其对公路的影响进行分析,最后对灾害成因及治理方法提出了建议。 相似文献
17.
18.
本文首先采用基于多准则决策的层次分析评价法,根据自然灾害风险理论,将洪涝风险影响因子分为危险性和脆弱性两类,子准则层包括平均降雨量、汇流累积量、坡度、海拔和土地覆盖度、道路级别、地表产流能力7个因子,构建了道路洪涝灾害风险评价模型。然后以福建省武夷山地区为研究区,利用地形数据、气象数据及遥感影像提取土地覆盖类型数据,通过道路洪涝灾害风险评价模型,绘制了道路风险分区图。结果表明,中、高风险积水道路占比较高,主要集中在东部、西部和中南部地区。本文对道路洪涝灾害风险所进行的评价,可服务于洪涝灾害风险预警和应急救援规划。 相似文献
19.
20.