ON THE FISSURE DEPOSITS OF CHINGHSINGHSIEN(井陘县) WITH REMARKS ON THE CENOZOIC GEOLOGY OF THE SAME AREA

In August 1933, the writers of the present paper were sent by the Geological Survey to Chinghsinghsien along the Chengtai Railway, on the Hopei and Shansi border, to examine the long known but not sufficiently surveyed     

ON SOME NEOLITHIC (AND POSSIBLY PALAEOLITHIC) FINDS IN MONGOLIA,SINKIANG AND WEST CHINA

In the course of the past two years,when they were in the field with theThird American (1930) and the Haardt-Citroen (1931) Central Asiatic Expedi-tions,the authors of the present note had opportunities for making a series ofarchaeological observations over an extensive area.It seems interesting to report     

ON THE GOBI PLANE OF DEFLATION—THE GOBI EROSION PLANE

Anyone Who travels in Mongolia cannot help being struck by a remarkable feature in the topography. Between the mountainous lands and the recently dissected basins the vast country of Mongolia is covered by a great number of separated or more or less continuous smooth surfaces at an inter-     

四川巴縣新開市和尚坡洞穴地層之發現及其意義

關於嘉陵江下游新生代地史,最近有一顯著之進步,卽重慶西之背斜層東翼,沿成渝公路之新開市附近和尚坡地方,有合骨化石洞穴層之發見。由此發見,使吾人對此區地史與地文之演變,得一古生物根據,從此而可修正以前若干解說,並可     

路南新生代地質

雲南各地,間山盆地甚多,路南即爲其一。路南盆地中主要地層爲紅色岩系。此等紅色岩系,以前地質學者,多視爲二疊紀上部(戴普拉)(安寧系朱庭祜)。二十六年卞美年於赴邱北途中,在路南城北約五里之山坡,獲得雷(?)及古豬與龜鳘類化石若干,首次證明路南有第三紀初期地層之存在。因時局關係,此項地層與化石之研究,均未能即時問世。邇來地質調查     

新採集之脊椎動物化石簡報

一年以來,關於新生代骨化石之採集與研究,續有進展。除賈蘭坡在四川,技工王存義在河北邢台西所獲標本爲前所採集,新經研究者外;關於第三紀初期者,李悅言在河南盧氏,卞美年在雲南曲靖及魯南,均獲有確切無疑之始新統或漸新統     

新生代地質研究与經濟地質

在地質研究中,新生代地質,向來是最易被人忽略的一部分,早年的地质報告中,提到第三纪第四纪地層,每以数十字成十餘字了之,最普遍的無非是紅色岩系或第三紀初期砂岩,三趾馬紅土或黄土等而已。一般的地质调查,多注意新生代以前地層,故此等现象,本無足怪。     

Spatiotemporal variations of cultivated land use efficiency in the Yangtze River Economic Belt based on carbon emission constraints

In this study,the carbon emissions(CEs)from cultivated land(CL)were included as an undesirable output in the utilization efficiency of such land.A slack-based model was used to calculate the CL use efficiency(CLUE)for 11 provinces and cities in the Yangtze River Economic Belt(YREB)from 2007 to 2016,and then a kernel density estimation map was drawn to analyze the spatiotemporal variations of CLUE.The Tobit model was also employed to analyze the factors affecting the CLUE.The results show the following.1)In the YREB,the CEs from CL showed a rising and then a slowly decreasing trend.In this paper,we calculate CEs by carbon emission factors and major carbon sources,and the CEs from CL in the YREB totaled 25.2354 million tons in 2007.By 2014,the value had increased gradually to 28.4400 million tons,and by 2016 it had declined to 27.8922 million tons,suggesting that the carbon-emission reduction measures of the government had an impact.2)The CLUE of various provinces and cities in the YREB showed an upward trend in the time dimension,while for the spatial dimension,the kernel density was high in the east and low in the west,and the areas with high kernel density were mainly located in the Yangtze River Delta.3)The per capita gross domestic product,the primary industrial output,and the number of agricultural technicians per 10,000 people had positive effects on the CLUE.The CL area per capita and the electrical power per hectare for agricultural machinery had significant negative impacts on CLUE.In addition,every 1%increase in the number of agricultural technicians increased the CLUE by 0.057%.     

国际气候变化研究趋势

以全球变暖为显著特征的气候变化现象引起了政府、公众和科学界的广泛关注。近年来,一系列极端气候事件更使气候变化成为一个全球性的重大议题。2009年哥本哈根会议中的争论表明,气候变化已经超出一般的环境或气候领域,是涉及到新的