全文获取类型
收费全文 | 214篇 |
免费 | 59篇 |
国内免费 | 80篇 |
专业分类
地球物理 | 21篇 |
地质学 | 314篇 |
海洋学 | 1篇 |
天文学 | 1篇 |
综合类 | 13篇 |
自然地理 | 3篇 |
出版年
2023年 | 3篇 |
2022年 | 5篇 |
2021年 | 8篇 |
2020年 | 6篇 |
2019年 | 9篇 |
2018年 | 7篇 |
2017年 | 9篇 |
2016年 | 13篇 |
2015年 | 7篇 |
2014年 | 14篇 |
2013年 | 17篇 |
2012年 | 16篇 |
2011年 | 6篇 |
2010年 | 13篇 |
2009年 | 22篇 |
2008年 | 11篇 |
2007年 | 14篇 |
2006年 | 13篇 |
2005年 | 17篇 |
2004年 | 10篇 |
2003年 | 16篇 |
2002年 | 13篇 |
2001年 | 16篇 |
2000年 | 14篇 |
1999年 | 14篇 |
1998年 | 14篇 |
1997年 | 7篇 |
1996年 | 8篇 |
1995年 | 5篇 |
1994年 | 4篇 |
1993年 | 3篇 |
1992年 | 3篇 |
1991年 | 2篇 |
1990年 | 4篇 |
1989年 | 5篇 |
1988年 | 2篇 |
1987年 | 1篇 |
1986年 | 2篇 |
排序方式: 共有353条查询结果,搜索用时 16 毫秒
41.
新疆哈密坡子泉地区首次发现的隐爆角砾岩筒处在塔里木板块北缘活动带卡瓦布拉克微板块之上,基底地层为前寒武系,盖层主要为石炭系,受NE向断裂带控制。隐爆角砾岩特征及产出环境相似于金伯利岩。 相似文献
42.
43.
在湖南衡东县铅锌矿观察到一种似鱼形的断层角砾。利用单个角砾即可指示断层两盘位移方向和断层面产状。作者认为它将为变质岩区矿田构造研究、为钻孔岩心研究和矿山坑道地质研究中确定断层位移方向带来方便。 相似文献
44.
45.
豫西南蒲塘金矿床地质特征及成因探讨 总被引:4,自引:0,他引:4
蒲塘金矿床属爆破角砾岩型,主成矿期温度236~318℃,主矿体受爆破角砾岩筒控制,含矿围岩蚀变及矿体变化规律明显,黄铁矿及黄铜矿是金的主要载体矿物。矿石中Au-Cu含量呈正消长关系,成矿物质主要来源于花岗岩,从花岗岩的侵入到矿床的形成,大体上经过了晚燕山期浅成初始岩浆侵入-爆破,超浅成强烈爆破及热液成矿三个阶段。 相似文献
46.
47.
山西阳高堡子湾金矿地质特征及找矿标志 总被引:1,自引:0,他引:1
堡子湾金矿位于华北地台北缘天镇断拱东部阳高凸起区,是与印支未--海西期火山一次火岩有关的隐爆角砾岩型金矿床。成矿物质主要来自重熔型岩源--石英二长(斑)岩,隐爆角砾岩为容矿岩石,与隐爆带总体走向平行的张扭性断裂为导矿构造,隐爆角砾岩的内部裂隙及角砾间隙,是良好的储矿构造。 相似文献
48.
Victor B. MAGLAMBAYAN Daizo ISHIYAMA Toshio MIZUTA Osamu MATSUBAYA Yohei ISHIKAWA 《Resource Geology》2001,51(2):107-116
Abstract: The disseminated Au‐Ag telluride Bulawan deposit, Negros island, Philippines, is hosted by dacite porphyry breccia pipes which formed in a Middle Miocene dacite porphyry stock. Electrum and Au‐Ag tellurides occur mostly as grains intergrown with or filling voids between sphalerite, pyrite, chalcopyrite, galena and tennantite. Calcite, quartz and rare dolomite are the principal gangue minerals. Four types of alteration were recognized in the deposit, namely; propylitic, K‐feldspar‐sericitic, sericitic and carbonate alteration. Carbonate alteration is correlatable to the gold deposition stage and occurs mostly along fault zones. The δ18O and δ13C compositions of calcite and dolomite in propylite zone and ore‐stage dacite porphyry breccia were determined. The δ18O values of calcite in propylitized andesite range from +12.2 to +14.7%, and their δ13C values range from ‐6.1 to ‐1.0%. The δ18O values of calcite and dolomite in sericite‐ and carbonate‐altered, mineralized dacite porphyry breccia and dacite porphyry rocks range from +15.1 to +23.1%, and the δ13C values of calcite and dolomite range from ‐3.9 to +0.9%. The δ18O and δ13C values of the hydrothermal fluids were estimated from inferred temperatures of formation on the basis of fluid inclusion microthermometry. The δ18O values of hydrothermal fluid for the propylitic alteration were calculated to be +8.5 ‐ +9.5%, assuming 375°C. On the other hand, the δ18O values of ore solutions for base metal and Au mineralization were computed to be +13.6 ‐ +14.6%, assuming 270°C. The hydrothermal fluids that formed the Bulawan deposit are dilute and 18O‐enriched fluids which reacted with 18O‐ and 13C‐rich wallrocks such as limestone. 相似文献
49.
Storm deposits and storm-generated coarse carbonate breccias on a pelagic outer shelf (South-East Basin, France) 总被引:2,自引:0,他引:2
Michel Seguret Alexis Moussine-Pouchkine Guilherme Raja Gabaglia & Frederic Bouchette 《Sedimentology》2001,48(2):231-254
Uppermost Jurassic limestones of the South‐East Basin (France) are organized into four facies associations that were deposited in four distinct zones: (1) peritidal lagoonal limestones; (2) bioclastic and reefal limestones; (3) pelagic lime mudstones; (4) lime mudstones/calcarenites/coarse breccias. Calcarenite deposits of zone 4 exhibit sedimentary structures that are diagnostic of deposition under wave‐induced combined flow. In subzone 4a, both vertical and lateral transitions from lime mudstone/calcarenite to breccia indicate in situ brecciation under wave‐cyclic loading. Breccias were produced by heterogeneous liquefaction of material previously deposited on the sea floor. Deposits in subzone 4a record relatively long periods (>400 kyr) of sedimentation below wave base, alternating with periods of deposition under wave‐induced currents and periods of in situ deformation. In this zone, storm waves were attenuated by wave–sediment interaction, and wave energy was absorbed by the deformation of soft sediment. With reference to present‐day wave attenuation, water depths in this zone ranged between 50 and 80 m. Landwards of the attenuation zone, in zone 3, storm waves were reduced to fair‐weather wave heights. Storm wave base was not horizontal and became shallower landwards. As a consequence, water depth and wave energy were not linearly related. On a small area of the seaward edge of subzone 4a, cobbles were removed by traction currents and redeposited in subzone 4b. There, they formed a 100‐m‐thick wedge, which prograded over 3 km and was built up by the stacking of 5‐ to 20‐m‐thick cross‐stratified sets of coarse breccia. This wedge records the transport and redeposition of cobbles by a high‐velocity unidirectional component of a combined flow. The increase in flow velocity in a restricted area is proposed to result from flow concentration in a channel‐like structure of the downwelling in the gulf formed by the basin. In more distal subzone 4c, the hydrodynamic effect of wave‐induced currents was quasi‐permanent, and brecciation by wave–sediment interaction occurred only episodically. This indicates that, seawards of the attenuation zone, hydrodynamic storm wave base was deeper than mechanical storm wave base. Uppermost Jurassic carbonates were deposited and soft‐sediment deformed on a hurricane‐dominated ramp of very gentle slope and characterized by a zone of storm wave degeneration, located seawards of a zone of sedimentation below wave base. 相似文献
50.
香炉碗子金矿床产于脆一韧性剪切带内,控矿围岩为火山隐爆角砾岩体,通过硫,铅,氢,氧,碳,锶等同位素及稀土元素的研究可以看出,该矿床是一个中,低温有大气水参与火山热液型金矿床,其火山岩岩浆属太古宙结晶基底重熔再造,壳幔混合型。 相似文献