全文获取类型
收费全文 | 152篇 |
免费 | 38篇 |
国内免费 | 66篇 |
专业分类
测绘学 | 1篇 |
大气科学 | 4篇 |
地球物理 | 49篇 |
地质学 | 188篇 |
海洋学 | 4篇 |
天文学 | 5篇 |
综合类 | 4篇 |
自然地理 | 1篇 |
出版年
2024年 | 1篇 |
2022年 | 8篇 |
2021年 | 12篇 |
2020年 | 13篇 |
2019年 | 14篇 |
2018年 | 5篇 |
2017年 | 9篇 |
2016年 | 9篇 |
2015年 | 7篇 |
2014年 | 10篇 |
2013年 | 10篇 |
2012年 | 8篇 |
2011年 | 6篇 |
2010年 | 11篇 |
2009年 | 10篇 |
2008年 | 9篇 |
2007年 | 6篇 |
2006年 | 6篇 |
2005年 | 10篇 |
2004年 | 6篇 |
2003年 | 9篇 |
2002年 | 9篇 |
2001年 | 7篇 |
2000年 | 12篇 |
1999年 | 7篇 |
1998年 | 5篇 |
1997年 | 8篇 |
1996年 | 7篇 |
1995年 | 1篇 |
1994年 | 5篇 |
1993年 | 8篇 |
1992年 | 1篇 |
1991年 | 3篇 |
1990年 | 1篇 |
1987年 | 2篇 |
1984年 | 1篇 |
排序方式: 共有256条查询结果,搜索用时 140 毫秒
251.
INTRODUCTIONSystematizationofknowledgeofspatialandtemporalrela tionsbetweenregionalmetamorphismanddeformationsresult ed ,atthebeginningof 1970s,indistinctionoftectonometa morphiccycles (TMC)whichreflectone actmanifestationofmetamorphismandaccompanyingendoge… 相似文献
252.
QIANGTANG MASSIF CRUST DEFORMATION FEATURES, DIFFERENCE AND ITS GENETIC MECHANISM STUDY 相似文献
253.
高龙穹窿构造是一断块穹窿,而不是"短轴背斜";控制近SN走向金矿化硅化角砾岩带的断裂构造,是典型的调整构造。高龙断块穹窿及其周边的NW向断层和SN向走向调整断层,是高龙金矿床的控矿构造系统。 相似文献
254.
Setsuya Nakada Hiroshi Shimizu Kazuya Ohta 《Journal of Volcanology and Geothermal Research》1999,89(1-4)
Following 198 years of dormancy, a small phreatic eruption started at the summit of Unzen Volcano (Mt. Fugen) in November 1990. A swarm of volcano-tectonic (VT) earthquakes had begun below the western flank of the volcano a year before this eruption, and isolated tremor occurred below the summit shortly before it. The focus of VT events had migrated eastward to the summit and became shallower. Following a period of phreatic activity, phreatomagmatic eruptions began in February 1991, became larger with time, and developed into a dacite dome eruption in May 1991 that lasted approximately 4 years. The emergence of the dome followed inflation, demagnetization and a swarm of high-frequency (HF) earthquakes in the crater area. After the dome appeared, activity of the VT earthquakes and the summit HF events was replaced largely by low-frequency (LF) earthquakes. Magma was discharged nearly continuously through the period of dome growth, and the rate decreased roughly with time. The lava dome grew in an unstable form on the shoulder of Mt. Fugen, with repeating partial collapses. The growth was exogenous when the lava effusion rate was high, and endogenous when low. A total of 13 lobes grew as a result of exogenous growth. Vigorous swarms of LF earthquakes occurred just prior to each lobe extrusion. Endogenous growth was accompanied by strong deformation of the crater floor and HF and LF earthquakes. By repeated exogenous and endogenous growth, a large dome was formed over the crater. Pyroclastic flows frequently descended to the northeast, east, and southeast, and their deposits extensively covered the eastern slope and flank of Mt. Fugen. Major pyroclastic flows took place when the lava effusion rate was high. Small vulcanian explosions were limited in the initial stage of dome growth. One of them occurred following collapse of the dome. The total volume of magma erupted was 2.1×108 m3 (dense-rock-equivalent); about a half of this volume remained as a lava dome at the summit (1.2 km long, 0.8 km wide and 230–540 m high). The eruption finished with extrusion of a spine at the endogenous dome top. Several monitoring results convinced us that the eruption had come to an end: the minimal levels of both seismicity and rockfalls, no discharge of magma, the minimal SO2 flux, and cessation of subsidence of the western flank of the volcano. The dome started slow deformation and cooling after the halt of magma effusion in February 1995. 相似文献
255.
Usu volcano (Hokkaido, Japan) is a dacitic volcano, known for its high production rate of lava domes and crypto-domes. It is thus a good target to study processes of volcanic dome evolution (upheaval and/or relaxation). We carried out repeated GPS and microgravity surveys on the three most recent domes of Mt. Usu (1910: Meiji Shinzan; 1943–1945: Showa-Shinzan and 1977–1982: Usu-Shinzan). The repeat period was 1 to 2 months and extended from October 1996 to June 1997. We also compare new data with results from former studies. More than 20 years after the start of Usu-Shinzan dome growth, there is still subsidence at a maximum rate of about 7 to 8 cm/year. The reasons for this subsidence are discussed. Repeated gravity surveys revealed an increase of gravity on the domes (about 60±10 microgal/year for Usu-Shinzan, about 15 microgal at Showa-Shinzan and 10 to 20 microgal for Meiji-shinzan); this gravity increase exceeds that expected due to subsidence. We discuss and interpret the excess gravity change in terms of a density increase in the edifice, caused by a combination of processes (contraction of the edifice, water level change, devesiculisation, cooling and magma intrusion). Quantification of these processes at Usu volcano may help to understand the processes of evolution at domes on other volcanoes such as Merapi (Indonesia), Unzen (Japan) or Montserrat (West Indies). 相似文献
256.
川西花岗- 伟晶岩型锂矿科学钻探:科学问题和科学意义 总被引:4,自引:0,他引:4
松潘-甘孜造山带是一条锂-铍-钽稀有元素超常富集的地带。针对锂矿资源上游勘探开发的瓶颈,实施川西锂矿3000m科学钻探,穿过变质岩、伟晶岩和花岗岩,建立多学科地壳锂柱。围绕"花岗-伟晶岩型锂矿的构造成因"、"与锂矿有关的花岗岩属性和成因类型"、"花岗岩与伟晶岩的关系及分异作用"、"稀有金属的"源-运-储-剥"过程"、"变形-变质-岩浆-成矿的造山过程:从热量耗损到锂的富集",以及"含稀有元素极端条件下微生物的特异性、多样性及与深度关系"等关键科学问题,实现为锂矿的找矿突破提供构造背景、制约要素、参考数据和科学依据,为找矿远景预测靶区提供科学标志,并力图建立创新性锂矿成因理论,具有重要的科学意义和应用价值。 相似文献