全文获取类型
收费全文 | 1075篇 |
免费 | 161篇 |
国内免费 | 287篇 |
专业分类
测绘学 | 130篇 |
大气科学 | 10篇 |
地球物理 | 82篇 |
地质学 | 956篇 |
海洋学 | 71篇 |
天文学 | 12篇 |
综合类 | 118篇 |
自然地理 | 144篇 |
出版年
2023年 | 20篇 |
2022年 | 37篇 |
2021年 | 34篇 |
2020年 | 50篇 |
2019年 | 49篇 |
2018年 | 41篇 |
2017年 | 46篇 |
2016年 | 46篇 |
2015年 | 31篇 |
2014年 | 80篇 |
2013年 | 56篇 |
2012年 | 55篇 |
2011年 | 80篇 |
2010年 | 69篇 |
2009年 | 68篇 |
2008年 | 54篇 |
2007年 | 62篇 |
2006年 | 57篇 |
2005年 | 52篇 |
2004年 | 59篇 |
2003年 | 33篇 |
2002年 | 44篇 |
2001年 | 45篇 |
2000年 | 50篇 |
1999年 | 43篇 |
1998年 | 43篇 |
1997年 | 30篇 |
1996年 | 30篇 |
1995年 | 18篇 |
1994年 | 29篇 |
1993年 | 25篇 |
1992年 | 28篇 |
1991年 | 13篇 |
1990年 | 10篇 |
1989年 | 12篇 |
1988年 | 3篇 |
1987年 | 8篇 |
1985年 | 2篇 |
1984年 | 1篇 |
1983年 | 2篇 |
1982年 | 3篇 |
1981年 | 1篇 |
1980年 | 2篇 |
1978年 | 1篇 |
1977年 | 1篇 |
排序方式: 共有1523条查询结果,搜索用时 15 毫秒
71.
《Chemie der Erde / Geochemistry》2021,81(2):125748
Although antimony (Sb) and arsenic (As) exhibit similar geochemical behavior and toxicity in the environment, growing evidence suggests that their water–rock interaction behavior in contaminated rivers is quite different. Twenty-nine river water samples were collected between September and November 2018 from contaminated rivers around an antimony mine in Hunan Province, China. The concentrations of As and Sb were inversely proportional to the water flow distance. The rates and magnitudes of Sb decrease were more prominent than those of As. Silicate mineral dissolution from rocks such as silicified limestone increased the As and Sb concentration of in-mine-district (IMD) water. Dissolution of carbonate minerals, ion exchange, and competitive adsorption were the major water–rock interactions, resulting in rapidly decreasing As and Sb concentration in IMD direct impacted water and IMD indirect impacted water. The behaviors of As and Sb during water–rock interaction were dissimilar for areas dominated by carbonate and silicate minerals. 相似文献
72.
《China Geology》2021,4(2):230-244
The giant Dahutang tungsten (W) deposit has a total reserve of more than 1.31 Mt WO3. Veinlet-disseminated scheelite and vein type wolframite mineralization are developed in this deposit, which are related to Late Mesozoic biotite granite. Four major types of alterations, which include albitization, potassic-alteration, and greisenization, and overprinted silicification developed in contact zone. The mass balance calculate of the four alteration types were used to further understanding of the mineralization process. The fresh porphyritic biotite granite has high Nb, Ta, and W, but low Ca and Sr while the Jiuling granodiorite has high Ca and Sr, but low Nb, Ta, and W concentrations. The altered porphyritic biotite granite indicated that the Nb, Ta, and W were leached out from the fresh porphyritic biotite granite, especially by sodic alteration. The low Ca and Sr contents of the altered Neoproterozoic Jiuling granodiorite indicate that Ca and Sr had been leached out from the fresh granodiorite by the fluid from Mesozoic porphyritic biotite granites. The metal W of the Dahutang deposit was mainly derived from the fluid exsolution from the melt and alteration of W-bearing granites. This study of alteration presents a new hydrothermal circulation model to understand tungsten mineralization in the Dahutang deposit. 相似文献
73.
《China Geology》2021,4(4):686-719
The Jiaodong Peninsula in Shandong Province, China is the world’s third-largest gold metallogenic area, with cumulative proven gold resources exceeding 5000 t. Over the past few years, breakthroughs have been made in deep prospecting at a depth of 500–2000 m, particularly in the Sanshandao area where a huge deep gold orebody was identified. Based on previous studies and the latest prospecting progress achieved by the project team of this study, the following results are summarized. (1) 3D geological modeling results based on deep drilling core data reveal that the Sanshandao gold orefield, which was previously considered to consist of several independent deposits, is a supergiant deposit with gold resources of more than 1200 t (including 470 t under the sea area). The length of the major orebody is nearly 8 km, with a greatest depth of 2312 m below sea level and a maximum length of more than 3 km along their dip direction. (2) Thick gold orebodies in the Sanshandao gold deposit mainly occur in the specific sections of the ore-controlling fault where the fault plane changes from steeply to gently inclined, forming a stepped metallogenic model from shallow to deep level. The reason for this strong structural control on mineralization forms is that when ore-forming fluids migrated along faults, the pressure of fluids greatly fluctuated in fault sections where the fault dip angle changed. Since the solubility of gold in the ore-forming fluid is sensitive to fluid pressure, these sections along the fault plane serve as the target areas for deep prospecting. (3) Thermal uplifting-extensional structures provide thermodynamic conditions, migration pathways, and deposition spaces for gold mineralization. Meanwhile, the changes in mantle properties induced the transformation of the geochemical properties of the lower crust and magmatic rocks. This further led to the reactivation of ore-forming elements, which provided rich materials for gold mineralization. (4) It can be concluded from previous research results that the gold mineralization in the Jiaodong gold deposits occurred at about 120 Ma, which was superimposed by nonferrous metals mineralization at 118–111 Ma. The fluids were dominated by primary mantle water or magmatic water. Metamorphic water occurred in the early stage of the gold mineralization, while the fluid composition was dominated by meteoric water in the late stage. The S, Pb, and Sr isotopic compositions of the ores are similar to those of ore-hosting rocks, indicating that the ore-forming materials mainly derive from crustal materials, with the minor addition of mantle-derived materials. The gold deposits in the Jiaodong Peninsula were formed in an extensional tectonic environment during the transformation of the physical and chemical properties of the lithospheric mantle, which is different from typical orogenic gold deposits. Thus, it is proposed that they are named “Jiaodong-type” gold deposits.©2021 China Geology Editorial Office. 相似文献
74.
75.
金川超镁铁质岩体矿物化学特征及矿物地质温度计、压力计研究 总被引:4,自引:0,他引:4
根据金川超镁铁质岩体主要造岩矿物和副矿物的共生组合关系及各种矿物的化学成分特点;选用5种较成熟、使用较方便的矿物地质温度计、压力计(主要是辉石温压计和角闪石压力计),对岩体形成的温、压条件进行了估算,其结果为:成岩温度为1000~1300℃(上限可到1400~1500℃),成岩压力约为5×10 ̄8~11×10 ̄8pa。金川超镁铁质岩体的主要岩石类型为尖晶石二辉橄榄岩,这一岩石类型在复杂体系相关系图中的稳定区域大致处于5×l0 ̄8~15×10 ̄8pa的范围,这与矿物温压计估算的成岩温压条件是一致的。 相似文献
76.
77.
78.
《矿产资源法》颁布实施五周年,通过宣传贯彻,增强了广大干部、群众依法办矿的法制观念,推动了各项矿管工作的开展,依法办矿的矿山取得了采矿权,非法采矿的小矿山被关闭,违法行为受到查处,矿管部门的声望越来越高,促讲了依法治矿。宣传贯彻《矿产资源法》要领导首先学法,提高认识,加强领导,建立一支专兼结合的宣传队伍,采取多种形式有重点地进行宣传教育。我国、我省面临矿产资源形势是严峻的,浪费矿产资源的现象仍存在,要继续深入宣传贯彻《矿产资源法》。 相似文献
79.
矿物包裹体中水溶气体成分的物理化学参数图解 总被引:8,自引:3,他引:8
本文计算出1m~3mNaCl体系.温度为100~500℃条件下CO_2、CH_4、H_2、CO、N_2、H_2S和SO_2亨利常数,以及上述成分在100~350℃时的分配系数和气、液平衡常数.并设计出矿物包裹体中水溶气体的lgfo_2—T、lgf_(co)-T、lgf_(co)-T和lgf_(co)-pH等物理化学参数图,解析了江西茅坪锡矿床中石英和锡石的矿物包裹体形成的物理化学条件. 相似文献
80.
Aggregates are produced from sand and gravel deposits or from bedrock sources. Production sites are numerous to minimize transport and are more and more in a competing land use position. Urbanization, while creating a market, also sterilizes deposits and pressures producers to relocate further from populated areas. Regulating and permitting quarries is an issue in regions with growing populations. This regulatory environment may cause exploitation schemes to evolve towards greater recycling, importing, and marine production, for example. These changes may be entirely attributable to increased environmental constraints on producing operations and not on conventional mining constraints such as overburden, ore grade, and costs of operation. 相似文献