青藏高原东南缘四姑娘山地区末次冰期砾石沉积和冰楔特征

四姑娘山位于青藏高原东南缘,第四纪冰川可分为3期.末次冰期时长坪沟口属于冰缘地带,在前次冰期冰碛物上发育了冰楔构造,冰缘地带冰川融水形成黑色细砾堆积.根据新的证据,末次冰期时四姑娘山长坪沟口附近年平均气温比现在低14～20℃.末次冰川作用发生时恰好也是四姑娘山地区强烈抬升的时期,因此,这套粗碎屑堆积可能是推覆构造的沉积响应,表明末次冰期时可能存在气候与构造联动作用.四姑娘山地区末次冰川规模较倒数第二次冰期明显偏小.     

Magnetic characteristics and their paleoclimatic significance of Fengzhou loess in the Qinling Mountains of China

The Fengzhou loess section is very typical in the Qinling Mountains. The section, about 82 m thick and underlain by the Neogene red clay, consists of 33 layers of loess and 33 layers of paleosol. The section covers Brunnes normal polarity zone and Matuyama reversed polarity zone, and the B/M boundary is located in the middle of L₈. Matuyama reversed polarity zone records Jaramillo, Olduvai and Reunion normal polarity subchrons. The boundary between Matuyama reversed polarity zone and Gauss normal polarity zone (M/Ga) appears in the lithological boundary between loess and the Neogene red clay. Loess accumulation in Fengzhou started before 2.48 Ma. The magnetic susceptibility curve indicates 33 cold-dry and humid-warm cycles of paleoclimatic variation in the Qinling Mountains during the last 2.48 Ma. The above climatic fluctuation may be well compared with that of the oxygen isotopic records from deep-sea deposits.     

AMS dating on glacial tills at the source area of the Urumqi River in the Tianshan Mountains and its implications

Using accelerating mass spectrometry (AMS) dating method, a dating has been made on the primary calcium carbonate in tills and secondary calcium carbonate coating on till gravel and the roche moutonnee formed since the Last Glaciation at the source area of the Urumqi River valley in the Tianshan Mountains, northwestern China. The results reveal that the carbonate content in the tills in this noncarbonate area is high enough to date by AMS, that the carbon in the coatings on the newly exposed roche moutons and in the modern till is modern carbon and so the¹⁴C dating results in the ancient till can represent the actual ages of the till formation, and that the warm period during the Holocene began as early as 6 500 a B. P. and lasted to 1 800 a B. P.     

华蓥山锶矿带构造控矿机理

华蓥山锶矿带是我国最重要的锶矿成矿带。在华蓥山大断裂及其以东的川湘台褶带区域构造变形机制研究的基础上，首次总结并提出了构造时、空演变规律及其对古构造环境、含矿岩系和锶矿的控制作用。     

创建太行山中段森林公园刍议

论证了创建太行山中段森林公园的必要性和可行性，分析了其发展的制约因素，并提出了创建森林公园的具体措施。     

山西太岳山植被地理

本文记述太岳山地区八个植被型,三十七个群系,并附1:500,000植被分布图。     

龙门山推覆构造变形特征

文章把龙门山推覆构造划分为4个推覆体和3个滑覆体。分别叙述了它们各自的变形特征。计算了造山带的地壳缩短率为42～63%。最后确认了龙门山推覆构造的推覆模式是推覆滑覆叠加模式,其发展方向为由北西向东南,扩展方式为背驮式(或前展式)。     

隐秀曲折悠然恬淡--浅析春晓园与山水田园诗歌

中国园林与诗歌有着渊源不断的联系。春晓园的园林设计中 ,从立意到构图 ,处处以唐代诗歌为蓝本 ,注意营造诗歌意境 ,表现出了较为明显的自然山水与人的融合。     

芦芽山珠芽蓼群落种间关联的研究

选取芦芽山珠芽蓼群落中的22个优势种,运用χ^2检验、Ochiai指数以及Spearman秩相关系数进行种间关联和种间相关的分析.结果表明,珠芽蓼群落整体上呈正关联,各种间相互依存.Spearman秩相关分析表明,优势种对间大多呈极显著或显著正相关,生态位重叠幅度较大.根据优势种种间相关性和种群的生态适应特征,将22个优势种分为2个生态种组,第二种组与第一种组间相关不显著,组内种对间相关显著.     

翠华山国家地质公园市场拓展策略研究

从市场认知的角度,采用定性分析方法,以"地质科学含义"为标准,对我国国家地质公园旅游开发现状进行分析,提出了浅认知度国家地质公园的概念,并对其进行了分类说明.在此基础上,以市场拓展为目标,提出了翠华山国家地质公园树立市场品牌形象的两点策略:一是通过"借势"和"挖潜"提升国家地质公园形象特色;二是通过有效融资、政府重视和提高管理水平形成市场拓展的有效支持.