全文获取类型
收费全文 | 191篇 |
免费 | 24篇 |
国内免费 | 74篇 |
专业分类
大气科学 | 7篇 |
地球物理 | 11篇 |
地质学 | 258篇 |
海洋学 | 4篇 |
天文学 | 1篇 |
综合类 | 3篇 |
自然地理 | 5篇 |
出版年
2023年 | 1篇 |
2022年 | 6篇 |
2021年 | 7篇 |
2020年 | 5篇 |
2019年 | 3篇 |
2018年 | 6篇 |
2017年 | 4篇 |
2016年 | 9篇 |
2015年 | 4篇 |
2014年 | 19篇 |
2013年 | 14篇 |
2012年 | 23篇 |
2011年 | 11篇 |
2010年 | 8篇 |
2009年 | 9篇 |
2008年 | 6篇 |
2007年 | 14篇 |
2006年 | 12篇 |
2005年 | 10篇 |
2004年 | 9篇 |
2003年 | 9篇 |
2002年 | 7篇 |
2001年 | 13篇 |
2000年 | 9篇 |
1999年 | 6篇 |
1998年 | 12篇 |
1997年 | 7篇 |
1996年 | 10篇 |
1995年 | 3篇 |
1994年 | 3篇 |
1993年 | 4篇 |
1992年 | 5篇 |
1991年 | 6篇 |
1990年 | 6篇 |
1989年 | 1篇 |
1988年 | 2篇 |
1987年 | 2篇 |
1986年 | 2篇 |
1985年 | 2篇 |
排序方式: 共有289条查询结果,搜索用时 0 毫秒
1.
思茅坳陷油气地质特征与勘探前景 总被引:2,自引:0,他引:2
思茅坳陷存在古生界和中一新生界两套沉积盖层,具有多套生储盖组合。以二叠系、三叠系为主力烃源岩,储层低孔低渗,侏罗系一白垩系“红层”组成区域盖层。思茅坳陷气水同喷、原油显示表明,该区海相地层仍有油气勘探前景,以存在K3-N区域盖层、断裂改造较弱、源岩成熟度较低、构造发育的英德一景谷、勐腊一勐满含油气保存单元为首选靶区,具有一定勘探前景。 相似文献
2.
云南红河县龙然村滑坡为—浅层牵引式破碎松散层滑坡,连续的降雨是诱发滑坡的主要因素.该滑坡的治理应采用“挡+排”的综合治理,“档”即在滑坡上缘设置抗滑桩、档板和毛石混凝土挡墙;“排”即沿滑坡顶、滑坡体两侧分别设置截水和排水沟,将地表水及雨水排出滑坡体外,以保证该滑坡体的稳定. 相似文献
3.
4.
成都粘土裂隙成因研究 总被引:1,自引:0,他引:1
赵翔 《地质灾害与环境保护》1997,8(4):40-46
根据成都粘土中裂隙特征与地质环境条件的分析,提出成都粘土中途中眩要裂隙类型的成因模式,上升剥蚀引起的垂向卸荷作用产生波状水平裂隙,冲沟切割引起的侧向卸荷作用,产生平行斜列隙裂。 相似文献
5.
利用1994年度《甘青交界祁连山西段水文地质工作空白区1∶50万区域水文地质调查》成果,结合空白区外以往资料,采用大气降水入渗法、地下水径流模数法和排泄量统计法等方法,对祁连山西段地下水天然资源进行了概算。结果是祁连山西段地下水天然资源总量为16.93亿m3/a,其中山地11.68亿m3/a,盆地5.25亿m3/a(已扣除重复量)。 相似文献
6.
双峰山金矿床地质特征及成因探讨 总被引:4,自引:0,他引:4
双峰山金矿产于双峰山背斜核部下石炭统巴塔玛依内山组第二亚组陆相火山岩内。即金矿化赋存于次生石英岩及蚀变安山岩中。金矿化与硅化、黄铁矿化关系密切,矿床具有Au、Ag、As、Sb、Hg等元素组合异常,表现出浅成低温热液矿化蚀变特征。提出了双峰山金矿为浅成低温热液型冰长石—绢云母金矿亚型矿床的成因认识。 相似文献
7.
Eloïse Gaillou Aurlien Delaunay Benjamin Rondeau Martine Bouhnik-le-Coz Emmanuel Fritsch Guy Cornen Christophe Monnier 《Ore Geology Reviews》2008,34(1-2):113
Seventy-seven gem opals from ten countries were analyzed by inductively coupled plasma-mass spectrometry (ICP-MS) through a dilution process, in order to establish the nature of the impurities. The results are correlated to the mode of formation and physical properties and are instrumental in establishing the geographical origin of a gem opal. The geochemistry of an opal is shown to be dependant mostly on the host rock, at least for examples from Mexico and Brazil, even if modified by weathering processes. In order of decreasing concentration, the main impurities present are Al, Ca, Fe, K, Na, and Mg (more than 500 ppm). Other noticeable elements in lesser amounts are Ba, followed by Zr, Sr, Rb, U, and Pb. For the first time, geochemistry helps to discriminate some varieties of opals. The Ba content, as well as the chondrite-normalized REE pattern, are the keys to separating sedimentary opals (Ba > 110 ppm, Eu and Ce anomalies) from volcanic opals (Ba < 110 ppm, no Eu or Ce anomaly). The Ca content, and to a lesser extent that of Mg, Al, K and Nb, helps to distinguish gem opals from different volcanic environments. The limited range of concentrations for all elements in precious (play-of-color) compared to common opals, indicates that this variety must have very specific, or more restricted, conditions of formation. We tentatively interpreted the presence of impurities in terms of crystallochemistry, even if opal is a poorly crystallized or amorphous material. The main replacement is the substitution of Si4+ by Al3+ and Fe3+. The induced charge imbalance is compensated chiefly by Ca2+, Mg2+, Mn2+, Ba2+, K+, and Na+. In terms of origin of color, greater concentrations of iron induce darker colors (from yellow to “chocolate brown”). This element inhibits luminescence for concentrations above 1000 ppm, whereas already a low content in U (≤ 1 ppm) induces a green luminescence. 相似文献
8.
9.
通过柴窝堡铜矿带区域沉积环境、构造环境及岩浆活动分析,认为矿带具备铜矿成矿地质条件.具体阐述了铜沟─庙儿沟铜矿田的成矿地质地球化学特征和矿化富集规律,认为铜沟─庙儿沟铜矿区的矿床属沉积─热液叠加改造型层控矿床. 相似文献
10.
P. Suneeta 《Marine Geodesy》2018,41(1):86-97
Several studies on tropical cyclone genesis potential index (GPI) mainly using atmospheric parameters (relative/absolute vorticity, relative humidity, vertical wind shear, potential instability, vertical velocity etc.) have been reported earlier. Though the ocean plays a vital role in the genesis and intensification of cyclones, no ocean parameter has been included in most of the studies. In this study, we have made an attempt to develop a new GPI for Bay of Bengal during peak post-monsoon (October-November) season including upper ocean heat content (UOHC) using the data for the period 1995–2015. It is found that the new GPI is better correlated with the total number of depressions, cyclones and severe cyclones (TNDC) compared with the existing GPI which was developed for the north Indian Ocean and presently used by India Meteorological Department (IMD), New Delhi. The correlation has significantly enhanced (r=0.86:significant at >99% level) by using the first differences [year(0) –year(?1)] of the time series data. Since, the new GPI which considers atmosphere and ocean (UOHC) parameters, it appears to be more suitable for Bay of Bengal during the peak post-monsoon season. 相似文献