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991.
拉尔玛金矿的生物成矿作用 总被引:1,自引:0,他引:1
位于甘、川两省交界处的拉尔玛金矿床,赋存于下寒武统太阳顶群,矿区内岩浆活动不强烈,矿床中断裂构造较发育,矿石矿物种类较齐全。矿石中的生物有机地球化学特征表明其为细菌和低等藻类生物体衍生的生物标志物和遗传特征,证明了太阳顶群中的有机质起源于菌藻类生物。矿石中的金属矿物生物组构有生物有机胶体组构和矿交代生物组构,说明生物成矿作用经历了直接成矿和间接成矿,即两轮聚矿作用,菌藻生物的第一轮聚金主要形成矿源层,生物的两轮聚金结果,形成此矿床。 相似文献
992.
为了更好地理解西北干旱区大气混合层(ML)厚度的变化特征及其对当地干旱气候形成的影响,我们利用张掖和民勤站夏季及相关月的实测探空资料及T-log P图解法,首先计算了该两地逐日ML厚度,然后分析并讨论了它的时空间变化特征、与干湿天气气候的关系,以及夏半年的深厚ML,对加剧当地干旱气候的影响.结果表明:(1)河西中东部ML厚度的年变化及地区差异明显.冬季最浅薄,夏半年深厚(特别是5、6月),4月及10月分别是ML急剧增厚及变薄的过渡期;同时,更靠近西北干旱区中心的河西西部及北部的ML更深厚.(2)夏季干(湿)天气通过加强(减弱)地气间的感热交换和干对流,而明显影响当地的ML厚度.平均而言,以高温日最深厚,千日次之,小雨日再次之,而中强雨日最浅薄.千年夏季的ML厚度平均比湿年的对应值增厚300 m左右.夏季典型千日的ML厚度比雨日厚3000 m,典型干日的ML厚度昼宿变化不大.(3)反过来夏半年深厚的ML也通过增加雨滴蒸发损耗,减少了干旱区的降水,加剧了当地干旱的程度,因此夏半年深厚的ML也是形成干旱气候背景的成因之一. 相似文献
993.
构造运动强烈、不断发生强震的云南地壳,可能经常有部分区域处于不稳定状态,外力也正是在此基础上才得以对地震活动显示出明显的调制效应。1988年11月6日澜沧—耿马7.6级、7.2级大地震前的大量观测资料表明,云南地区,特别是澜沧—耿马附近地区又再次出现了类似1970年通海7.7级、1974年大关7.1级和1976年龙陵7.4级大地震之前,曾发生过的那种地表涝旱剧变和大气压力巨涨落现象。这种震前的外部异常扰动具有很强的重复性,在对应地震上也显示了很强的应验性,故其很有可能在云南未来7级大地震的监视预报中发挥作用。 相似文献
994.
Michael P.RICHARDS 《中国科学D辑(英文版)》2009,52(1):85-92
Despite great achievements in the origins of domestic pigs made by the methods of zooarchaeology and molecular biology, how
to scientifically distinguish the domesticated pigs from wild boars during the early stage of pig domestication is still poorly
understood. Compared to wild boar’s diets which come from the natural environment, the diets of domestic pigs are more easily
influenced by human feeding activities. Therefore, in principle, exploration of the dietary differences among pigs and under-standing
the impact on pig diets fed by humans can have great potential to differentiate between wild boars and domesticated pigs.
To reveal dietary differences among pigs and distinguish the domesticated pigs from wild boars based on comparison with the
diets of humans and other animals, we analyzed the carbon and nitrogen stable isotopes of human bones from Xiaojingshan Site
and animal bones from Yuezhuang Site, both of which belong to Houli Culture in Shandong Province and date to about 8500-7500
years ago. The mean δ13C value ((−17.8 ± 0.3)‰) and δ15N value ((9.0±0.6)‰) in human collagen indicate that although millet agriculture began it was not the main subsistence strategy
as millets are typical of C4 plants and that humans made a living mainly by gathering, hunting or raising some domesticated animals. The δ13C value (−16.1‰) and δ15N value (6.9‰) in the bovine suggest that C3 plants were dominant in its diet with some C4 plants complemented. The fish has lower δ13C value (−24.9‰) and higher δ15N value (8.8‰) than the bovine, which is the characteristic of the isotopic values from Eurasian freshwater fish. Based on
the differences in carbon and nitrogen isotope values, the pigs can be divided into three groups. A group, composed of two
pigs, has low δ13C values (−18.1‰, −20.0‰) and low δ15N values (4.7‰, 6.0‰). B group, only one pig, has the highest δ13C value (−10.6‰) and mediate δ15N value (6.4‰). As for the C group, also only one pig, low δ13C value (−19.0‰) and the highest δ15N value (9.1‰) are observed. Previous studies on the stable isotopes from modern or ancient wild boars’ bones have suggested
that C3 plants are predominated in their diets and that their δ15N values are close to those in herbivores and far from those in carnivores. Based on the comparison with the isotope values
from humans, the wild boars and the domestic pigs from Xipo Site in Henan 6000-5500 years ago and Kangjia Site in Shaanxi
4500-4000 years ago, we conclude that A pig group belongs to wild boars while B and C groups can be attributed to domesticated
pigs.
Supported by Max-Planck Society and Chinese Academy of Sciences, Knowledge Innovation Program of the Chinese Academy of Sciences
(Grant No. KJCX3.SYW.N12), National Natural Science Foundation of China (Grant No. 40702003) and President Funding of Graduate
University of Chinese Academy of Sciences 相似文献
995.
福建顺昌尾波Q值衰减特征初探 总被引:1,自引:0,他引:1
基于Sato单次散射模型,利用2007年3月13日福建数字地震台网记录的发生在福建省北部地区的45条ML≥2.0级地震波形资料,对福建北部地区尾波Q值进行了研究,研究中首先计算各条记录尾波4—18Hz间15个频率的尾波Q值,并对Q值与频率之间的依赖关系进行拟和,拟和结果为:Qc(f)=(150.34±42.51)f^(0.8214±0.2109)。 相似文献
996.
Two stages of isotopic exchanges experienced by the Ertaibei granite pluton, northern Xinjiang, China 总被引:1,自引:0,他引:1
LIU Wei 《中国科学D辑(英文版)》2000,43(6):605-616
18O/16O and D/H of coexisting feldspar, quartz, and biotite separates of twenty samples collected from the Ertaibei granite pluton,
northern Xinjiang, China are determined. It is shown that the Ertaibei pluton experienced two stages of isotopic exchanges.
The second stage of18O/16O and D/H exchanges with meteoric water brought about a marked decrease in the δ18O values of feldspar and biotite from the second group of samples. The D/H of biotite exhibits a higher sensitivity to the
meteoric water alteration than its18O/16O. However, the first stage of18O/16O exchange with the18O-rich aqueous fluid derived from the dehydration within the deep crust caused the Δ18OQuartz-Feldspar reversal. It is inferred that the dehydration-melting may have been an important mechanism for anatexis. It is shown that
the deep fluid encircled the Ertaibei pluton like an envelope which serves as an effective screen to the surface waters. 相似文献
997.
Surface water oxygen and hydrogen isotopic values are commonly used as proxies of precipitation isotopic values to track modern hydrologic processes while proxies of water isotopic values preserved in lake and river sediments are used for paleoclimate and paleoaltimetry studies. Previous work has been able to explain variability in USA river‐water and meteoric‐precipitation oxygen isotope variability with geographic variables. These studies show that in the western United States, river‐water isotopic values are depleted relative to precipitation values. In comparison, the controls on lake‐water isotopic values are not well constrained. It has been documented that western United States lake‐water input values, unlike river water, reflect the monthly weighted mean isotopic value of precipitation. To understand the differing controls on lake‐ and river‐water isotopic values in the western United States, we examine the seasonal distribution of precipitation, evaporation and snowmelt across a range of seasonality regimes. We generate new predictive equations based on easily measured factors for western United States lake‐water, which are able to explain 69–63% of the variability in lake‐water hydrogen and oxygen isotopic values. In addition to the geographic factors that can explain river and precipitation values, lake‐water isotopic values need factors related to local hydrologic and climatic characteristics to explain variability. Study results suggest that the spring snowmelt runs off the landscape via rivers and streams, depleting river and stream‐water isotopic values. By contrast, lakes receive seasonal contributions of precipitation in proportion to the seasonal fraction of total annual precipitation within their watershed. Climate change may alter the ratio of snow to rain fall, affecting water resource partitioning between rivers and lakes and by implication of groundwater. Paleolimnological studies must account for the multiple drivers of water isotopic values; likewise, studies based on the isotopic composition of fossil material need to distinguish between species that are associated with rivers versus lakes. Copyright © 2010 John Wiley & Sons, Ltd. 相似文献
998.
完备震级是评估区域地震台网检测能力的一个定量指标,本文采用能反映区域地震台网检测能力的时空分布细节特征的概率完备震级分析方法,对首都圈地震台网的检测能力进行了研究,通过对首都圈2002-2009共8年的地震目录和台站资料的分析处理,得到了首都圈地震台网的完备震级时空分布,据此对台网的检测能力进行了评估,并结合模拟结果探讨了提升台网检测能力的可能性.结果表明:首都圈地震台网的整体检测能力较强,北京地区的检测能力尤其突出,但部分区域检测能力仍有一定的提升空间;模拟结果表明,在东北、西北、西南等位置增加台站可能有助于进一步提高台网的检测能力.相关研究结果可能对未来首都圈地震台网的优化具有参考意义. 相似文献
999.
分析百度地图位置解析技术功能及特点,提出使用地址解析及坐标转换功能,对地震应急基础属性数据进行解析,实现基础属性数据空间化,设计地理坐标纠偏算法,提高地震应急基础数据的可用性,为地震应急工作提供数据保障。该算法操作简单,运行快捷,解决了地震应急基础数据库中属性数据及时更新的关键技术问题。 相似文献
1000.
随着地铁轻轨的迅速发展,我国大多数地电阻率测项受到不同程度干扰,诸多学者为此提出采用小波方法进行滤波的建议。文中拟采用小波和HHT滤波方法,以受津滨轻轨干扰严重的塘沽地电阻率观测资料为例,进行降噪处理,对比2种方法的滤波效果,以获得更好的滤波方法。 相似文献