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131.
库车盆地古近纪—新近纪时期具有巨厚的蒸发岩沉积,古近纪时期岩盐沉积的最大厚度达1 447.5 m,新近纪时期岩盐沉积的厚度有所减小,岩盐层最大厚度402 m。库车盆地在古近纪—新近纪时期沉积沉降中心也有所改变,从盆地西部的拜城凹陷转移到东部的康村—阳霞地区。库车盆地东西部蒸发岩岩体特征的差异,对此地区油气藏规模造成一定影响。初步判断库车盆地西部蒸发岩有可能比东部蒸发岩盐下形成的油气藏量较大。盆地中蒸发岩沉积中心的迁移对钾盐沉积也有重要影响。 相似文献
132.
W. A. Ambrose C. Breton M. H. Holtz V. Núñez-López S. D. Hovorka I. J. Duncan 《Environmental Geology》2009,57(7):1537-1551
Documenting geographic distribution and spatial linkages between CO2 sources and potential sinks in areas with significant levels of CO2 emissions is important when considering carbon-management strategies such as geologic sequestration or enhanced oil recovery
(EOR). For example, the US Gulf Coast overlies a thick succession (>6,000 m [>20,000 ft]) of highly porous and permeable sandstone
formations separated by thick, regionally extensive shale aquitards. The Gulf Coast and Permian Basin also have a large potential
for EOR, in which CO2 injected into suitable oil reservoirs could be followed by long-term storage of CO2 in nonproductive formations below reservoir intervals. For example, >6 billion barrels (Bbbl) of oil from 182 large reservoirs
is technically recoverable in the Permian Basin as a result of miscible-CO2 flooding. The Gulf Coast also contains an additional 4.5 Bbbl of oil that could be produced by using miscible CO2. Although the CO2 pipeline infrastructure is well-developed in the Permian Basin, east Texas and the Texas Gulf Coast may have a greater long-term
potential for deep, permanent storage of CO2 because of thick brine-bearing formations near both major subsurface and point sources of CO2. 相似文献
133.
Indoor radon mapping and its relation to geology in Hungary 总被引:2,自引:0,他引:2
Mihály Minda György Tóth István Horváth Ivan Barnet Krisztián Hámori Eszter Tóth 《Environmental Geology》2009,57(3):601-609
Indoor radon mapping may show stronger dependence on geological formations if the measured homes are one-storied houses with
no basement. In Hungary, 17,244 homes were investigated on the yearly average of indoor radon concentrations; among these
homes, there were 6,154, one-storied, no-basement houses. In Hungary, 21 geological units were created relevant for indoor
radon index characterized by lithology, the position of the ground water table, and the gas permeability. Maps were drawn
of different topography (counties, grid, geological units) and different values (maximum, mean, indoor radon indexes). A kind
of standardization of houses was that only the one-storied, no-basement ones were chosen, but from geological point of view some more information was gained when the wall materials (bricks or adobe) were also taken
into account. (“Adobe” is made of clay and straw in Hungary, and not burned as brick, just dried on sunshine). Enhanced indoor
radon values can be observed on the bedrock of Cenozoic volcanic rocks and their eroded materials deposited on the local alluvial
valleys. Another group with relatively increased indoor radon values can be connected to granite bodies. The grid method is
useful for covering large state or even continental areas. For practical public use and detailed radon risk mapping geological
or administrative unit-systems could yield more reasonable and useful results. 相似文献
134.
135.
Nejib Jemmali Larbi Rddad Fouad Souissi Emmanuel John M. Carranza 《Comptes Rendus Geoscience》2019,351(4):312-320
Jebel Mecella and Sidi Taya F–(BaPbZn) deposits are located within the Fluorite Zaghouan Province (NE Tunisia). The mineralization occurs along the unconformity surface between the Jurassic limestones and Upper Cretaceous rocks. The mineralization consists mainly of fluorite, barite, sphalerite, and galena. The δ34S values of barite at Jebel Mecella (14.8–15.4‰) and at Sidi Taya (21.6–22.2‰) closely match those of the Triassic evaporites and Messinian seawater, respectively. The range of δ34S values of galena and sphalerite in both deposits (?6.9 to +2.4‰) suggests the involvement of thermochemical sulfate reduction and possibly organically-bound sulfur in the generation of sulfur. Lead isotope data with 206Pb/204Pb, 207Pb/204Pb, and 208Pb/204Pb ratios of 18.893–18.903, 15.684–15.699, and 38.850–38.880, respectively suggests a single homogeneous source reservoir of Paleozoic age and/or the homogenization of the Paleozoic–Cretaceous multireservoir-derived fluids along their long migration paths to the loci of deposition during the Alpine orogeny. 相似文献
136.
Jiawei Zhang Taiping Ye Yaran Dai Jianshu Chen Hui Zhang Chuangu Dai Guohua Yuan Kaiyuan Jiang 《地学前缘(英文版)》2019,10(5):1823-1839
The Neoproterozoic Tonian strata(ca.870-725 Ma)in the western Jiangnan Orogen archive the records of sedimentary provenance and tectonic setting which can be used to understand the geological evolution of the South China Continent.These strata are separated into the basement and cover sequences by a regional angular unconformity.The basement sequence can be subdivided into the lower and the upper parts by the widespread interbedded ca.840 Ma basalt with pillow structure.In the present work,234 concordant detrital zircon analyses are obtained from three Tonian sandstone samples in the Fanjingshan district,Guizhou Province.Combined with previous results,a total of 1736 analyses of detrital zircon U-Pb ages derived from 12 formations of Tonian strata in the western Jiangnan Orogen are used to decipher the integrated sedimentary and tectonic histories.The zircons from the lowermost part of the basement sequence(the Yujiagou Formation)show oval morphology and display two Paleoproterozoic age peaks at 2325 Ma and 1845 Ma which are similar with the detrital zircon age peaks from the Late Paleoproterozoic to Early Mesoproterozoic Dongchuan/Dahongshan/Hekou groups,suggesting a passive margin basin in which the sediments were mainly sourced from the southwestern Yangtze Block.However,the zircon age population of the lower part of the basement sequence(the Xiaojiahe,Huixiangping formations and their equivalents)indicates the sedimentary derivation from bidirectional sources(the ca.870 Ma arc materials in the south and the old detritus from the southwestern Yangtze Block)which is consistent with a back arc setting for the deposition of the sediments.Zircons from the upper part of the basement sequence(the Duyantang Formation and its equivalent)show euhedral and subangular morphology and display a unimodal age peak at ca.835 Ma.This sequence was possibly deposited in a convergent setting and the detritus were came from the locally distributed syn-collisional igneous rocks.The lower part of the cover sequence(the Xinzhai and Wuye formations and their equivalents)shows a distinct zircon age peak at 815—809 Ma and two subordinate peaks at 2485 Ma and 2018 Ma,suggesting that the basin had gradually transformed into a continental rift basin and received the detritus from the ca.815 Ma post-collisional magmatic rocks as well as from different Paleoproterozoic source rocks in the northern Yangtze Block.We propose a tectonic evolution model that envisages eruption of ca.840 Ma basalt in a back arc basin that existed during ca.870-835 Ma,an angular unconformity was formed during amalgamation of the Yangtze Block and the Cathaysia Block at ca.835-820 Ma and the rifting of the South China Continent was initiated at ca.800 Ma.Our study concludes that the South China Continent was formed on the periphery of the Rodinia supercontinent. 相似文献
137.
《China Geology》2019,2(1):56-66
Madagascar becomes a large isolated island after its dislocation from East Africa at its western part during the opening of the Mozambique Channel and its separation from India at its eastern part during the opening of the basin of the Mascarene. From a stratigraphic point of view, Karroo of Madagascar shares substantial similarities with the stratigraphic strata of East Africa. While oil companies have taken a liking to the basins of East Africa, they also turn to the basins in the western part of Madagascar especially after the discovery of large oil fields at Tsimiroro and Bemolanga. According to the study of their geological history, the basins of Madagascar contain huge hydrocarbon potential. The western basins, which is more developed than the east coast of the island, have been the subject of many in-depth studies by numerous researchers. The cross-referencing of bibliographic data with geological studies, and knowledge of hydrocarbon formation and maturation stages, carried out in this study served to determine the nature of source rocks, reservoir rocks, bedrock and eventual trapping system of hydrocarbons in Madagascar. This study identified the properties of Madagascar source rocks, reservoir rocks, bedrock and the final oil and gas trap system by cross-referencing the literature and geological research, oil and gas formation and maturity stages, and shows that Madagascar has considerable hydrocarbon potential.©2019 China Geology Editorial Office. 相似文献
138.
在定义地质档案资料范畴的基础上,阐述了在依法做好地质档案资料汇交工作中要注意做好几个方面工作的同时,重点论述了如何开展馆藏地质档案资料的开发利用工作,并在此基础上提出了宣传型、服务型、编辑型、技术型、转化型及计算机型等6种具体的开发地质档案资料的方式方法,以达进一步开发利用地质档案资源之目的.使其更好地为地质找矿、科研、教学及国民经济建设服务. 相似文献
139.
140.
从人类发展需要及科学理论趋势出发论述地球科学各门类的大体系综合理论跃迁的观点。提出以地球深源岩浆热动力为主链的岩石圈、水圈、大气圈和生态环境圈的总体物质——热力运动高统帅性理论。展望新的高技术观(监)测系统。 相似文献