共查询到20条相似文献,搜索用时 31 毫秒
1.
Hydrogen Isotopes of Glassy and Phyllosilicate Spherules in Al Rais (CR) and Orgueil (CI) Chondrites
Michael E.ZOLENSKY 《《地质学报》英文版》2004,78(5)
The hydroxyl in phyllosilicate minerals is the most common occurrence of water in primitive meteorites. Direct hydrogen isotopic analysis of this water component using an ion microprobe has been made in some glassy or phyllosilicate spherules from the Al Rais (CR) and Orgueil (CI) chondrites. The spherules from Al Rais show large deuterium excesses (δD = +200 -+800‰) relative to terrestrial standards, whereas deuterium-enrichments in the spherules from Orgueil are much smaller (δD = +40 - +130‰). The phyllosilicate spherules are products of 相似文献
2.
W. David SINCLAIR 《地质学报》2014,88(Z2):463-465
Please refer to the attachment(s) for more details. 相似文献
3.
4.
5.
Yu Zuxiang Institute of Geology Chinese Academy of Geological Sciences Beijing 《《地质学报》英文版》1997,71(2):152-157
Malanite was first found in veinlets of disseminated copper-nickel ores inZunhua County, Hebei Province, and then in platinum-bearing chromite ores in ShuangfengVillage, Yanshan. In the former case, malanite appears as octahedrons or dodecahedrons asso-ciated with pyrrhotite, pentlandite, sperrylite and cooperite; while in the latter case, it is massiveor present in anhedral glomerocrysts, filling in cracks of iridisite and associated with osmiride,ferrian platinum and iridisite. Malanite is steel-grey in colour, opaque with metallic lustre andblack streaks and brittle with no magnetism. H_M=5.0, VHN_(20)=417kg/mm~2, cleavage {111}sometimes observed. The calculated density is 7.57g/cm~3. The reflective colour is white with alight green tint. Internal reflections are not observed. This mineral is isotropic, showing nobireflection or reflection pleochroism in air. By means of electron microprobe analysis, the em-pirical formula (based on 7 atoms) is expressed as (Cu_(0.93)Fe_(0.06))_(∑0.99)(Pt_(1.03)Ir_(0.66)Rh_(0.04)Pd_(0.03)Co_(0.20)Ni_(0.03))_(1.99)S_(4.03) or (Cu_(0.95)Fe_(0.07))_(∑1.02)(Pt_(1.37)Ir_(0.45)Co_(0.11)Rh_(0.08))_(∑2.01)S_(3.97). Five strongestlines (hkl, d, I) of X-ray powder diffraction data of malanite are 311,2.98(6); 400,2.48(5);333, 1.90(7); 440, 1.75(10); 731, 1.29(5). It was known on the basis of X-ray powder diffractiondata that malanite is cubic, and the space group is Fd3m with α=0.9940nm, V=0.9821(3)nm~3 and Z=4. The type material of malanite is deposited at the Geological Museum of China(GMC)s 相似文献
6.
Helmut Tenzer Chan-Hee Park Olaf Kolditz Christopher Ian McDermott 《Environmental Earth Sciences》2010,61(4):853-880
Earth-reservoirs are increasingly exploited today with the extraction of resources, such as heat and hydrocarbons, and the
large-scale emplacement of waste, such as CO2 sequestration. The characterization, site investigation, predictive modeling and long-term monitoring are dependent on the
processes being investigated and modeled. In most cases complex coupled processes have to be addressed in a geologically complex
rock mass system. In this paper we present a conceptual holistic framework known as geomechanical facies linking all the scales
of investigation, characterization and reservoir development methods. We demonstrate this concept on the work undertaken during
the design and development of the enhanced geothermal systems (EGS) systems at the forefront of European Hot-Dry-Rock (HDR)
technology, Soultz-sous-Forêts (France) and Spa Urach (Germany). Soultz-sous-Forêts is situated within granitic rocks and
an active tectonic graben system in the central part of the Rhine Graben. It presents conditions of lithology, temperature,
stress, hydraulics and geochemistry that are very different from those at Spa Urach, located in a very dense gneiss formation
in the South German crystalline complex. Spa Urach exhibits more elastic behavior and is set tectonically within an almost
inactive strike-slip stress field described in more detail in Sects. “Drill core analysis” and “Hydraulic stimulation at Spa Urach”. This paper compares the exploration and field development methods used at these two sites against the back drop of the
geomechanical facies concept. Issues addressed include the key parameters for flow and heat transport properties, coupled
hydro-mechanical process identification, the success of the HDR reservoir as a heat exchanger and exploration techniques applicable
to the different facies. Identification of the key geomechanical facies gives an indication as to which technologies will
prove more efficient in the application of HDR technology. The results of this study will hopefully help in developing heat
recovery schemes for the long-term economical operation of future HDR plants and EGS as well as assist in the understanding
of engineered geosystems. 相似文献
7.
Peter Adamu Shivee Ranjanee Kaliappan Abdalla Sirag Ruth John Chenbap 《GeoJournal》2017,82(2):369-377
This study investigates the convergence of well-being between Sub Saharan Africa (SSA) and Organization for Economic Cooperation and Development (OECD) member countries during the period 1980–2014. The gap in living standard was examined from a steady state represented by the average income of OECD countries. Applying the unit root estimation technique to test for convergence with and without structural breaks, the result shows that; among a total of 43 countries studied, about 14 % are converging towards the average of OECD average. When the shock caused by the economic crisis of 2008 was factored into the analysis, the gains of about five countries out of the six converging disappeared. These results are disturbing owing to the fact that countries in the Asian region that started almost at the same level with SSA have converged to form a convergence club. Therefore, a lot more effort is needed from the government and stake holders in most countries in SSA to improve on the determinants of growth like good health care, quality institutions, better education and commitments to pursue developmental programmes which will boost the income of an average African to acquire better life. 相似文献
8.
Andreeva O. A. Yarmolyuk V. V. Savatenkov V. M. Andreeva I. A. Lebedev V. A. Ji J.-Q. Zhou X. 《Doklady Earth Sciences》2022,506(1):641-649
Doklady Earth Sciences - Changbaishan and Wang-Tian’e volcanoes of Changbaishan area (Northeast China) were formed with a slight time gap in the last four million years. Wang-Tian’e... 相似文献
9.
T. K. Zlobin 《Doklady Earth Sciences》2018,480(1):599-601
The peculiarities of catastrophic earthquakes that occurred in the Northwest Pacific region on January 13, 2007, and January 15, 2007, east of the Kuril Islands and the Tohoku megaearthquake of March 11, 2011, east of Japan are considered and analyzed. It is revealed that these earthquakes, apart from the fact that they occurred in the transition zone from the Pacific to island arcs and the Eurasian continent, have common features and similar characteristics. The seismotectonic slip in the source of the chronologically first event, the 2006 Kuril earthquake, was a gentle thrust, while that of the second event of January 13, 2007, was a downthrow beneath the Kuril deep trench. 相似文献
10.
11.
Geology of Ore Deposits - Paragenetic associations of tetrahedrite-(Zn) and sphalerite are distinguished in the Teremki gold-ore deposit. The chemical composition of coexisting minerals of this... 相似文献
12.
YU Wenhui and LIU Congqiang The State Key Laboratory of Environmental Geochemistry Institute of Geochemistry Chinese Academy of Sciences Guiyang Guizhou Graduate School of Chinese Academy of Sciences Beijing 《《地质学报》英文版》2005,79(3):343-348
1 Introduction Coherent element pairs (Y3+-Ho3+, Zr4+-Hf4+, Nb5+-Ta5+ and Sr2+-Eu2+) have the same valences and very similar ionic radii. They are seldom fractionated during silicate mineral/melt interaction systems because the partitioning of these element pairs between melts and minerals is tightly controlled by charge valence and crystal structure (lattice site size) or ionic radius. The concentration ratios of these pairs in igneous rocks are close to the chondritic values (Y/Ho=28, Zr… 相似文献
13.
正IGCP 630 and its Structures IGCP 630, with its full title of "Permian–Triassic(P–Tr) climatic and environmental extremes and biotic response", is an International Geoscience Program project sponsored by the United Nation Educational, Scientific Cultural Organization(UNESCO) and International Union of Geological Sciences(IUGS). This project was approved in 2014 and ended in 2018, and has applied for one-year 相似文献
14.
1IntroductionAuriferousquartzveinsarecommonintheFengyangandZhangbalingregionsofAnhuiProvinceandtheyconstitutetheRongdu ,Zhuding ,Dagongshan ,MaoshanandShangchenggolddepositsandalotofgoldperspectives .TheRb SrisochronagesofalterationmineralsfromtheRongduandDagongshangolddepositsare (10 9.0± 4 .4 )Maand (15 3.76± 11.2 )Ma ,respectively (Dongetal .,1995 ) .Thereisalargedifferenceinagebetweenthetwogolddeposits ,butitcanbeseenthatthegolddepositswereformedinLateJurassictoEarlyCretaceous .A… 相似文献
15.
Paleogeographical Distribution and Stratigraphical Range of the Lower Triassic Claraia,Pseudoclaraia and Eumorphotis(Bivalvia) 总被引:1,自引:0,他引:1
Yin Hongfu 《中国地质大学学报(英文版)》1990,(1)
On the basis of a worldwide review of Claraia,Pseudoclaraia andEumorphotis,especially their important species,two range zones are recog-nized:the Pseudoclaraia wangi range zone——Upper Griesbachia——and the Claraia stachei-C.aurita-Eumorphotis multiformis acme zone——Upper Griesbachian to Lower Smithian .This result revises both the traditional Chinese concept regarding these fossils as limited in Lower Scythian andthe viewpoint of some Eurasian researchers who hold Eumorphotis multifor-mis to be Upper Scythian.The paleogeographical distribution of the three genera is controlledprimarily by temperature(latitude)and secondarily by physiographic separa-tions.Distribution of these fossils is subdivided into four realms and five prov-inces.The Eastern Asia province of the Tethys realm is suggested as thesource area of these fossils.The striking contrast between the composition ofthe species along the southern and northern margins of the Tethys,togetherwith other distributional characters,supports the pla 相似文献
16.
Please refer to the attachment(s) for more details 相似文献
17.
18.
Soft corals and black corals are useful proxy tools for paleoceanographic reconstructions. However, most work has focused on deep-water taxa and few studies have used these corals as proxy organisms in shallow water (<200 m). To facilitate the use of stable nitrogen and carbon isotope (δ15N and δ13C) records from shallow-water soft coral and black coral taxa for paleoceanographic reconstructions, quantification of the inherent variability in skeletal isotope values between sites, across depth, and among taxa is needed. Here, skeletal δ15N and δ13C values were measured in multiple colonies from eleven genera of soft corals and two genera of black corals from across a depth transect (5-105 m) at two sites in Palau located in the tropical western Pacific Ocean. Overall, no difference in skeletal δ15N and δ13C values between sites was present. Skeletal δ15N values significantly increased and δ13C values decreased with depth. This is consistent with changes in isotope values of suspended particulate organic matter (POM) across the photic zone, suggesting that the primary food source to these corals is suspended POM and that the stable isotopic composition of POM controls the skeletal isotopic composition of these corals. Thus, to compare the isotope records of corals collected across a depth range in the photic zone, first order depth corrections of −0.013‰ m−1 and +0.023‰ m−1 are recommended for δ15N and δ13C, respectively. Average depth-corrected δ15N values were similar between black corals and soft corals, indicating that corals in these orders feed at a similar trophic level. In contrast, average depth-corrected δ13C values of black corals were significantly lower than that of soft corals, potentially resulting from metabolic processes associated with differing skeletal compositions among the orders (i.e., gorgonin vs. chitin based). Thus, a correction of +1.0‰ is recommended for black corals when comparing their δ13C-based proxy records to soft corals. After correcting for both the depth and order effects, variability in δ15N values among corals within each genera was low (standard deviation (SD) of the mean <±0.5‰), with the exception of Acanthorgorgia. The calculated SD of <±0.5‰ provides a first order guideline for the amount of variability that could be expected in a δ15N record, and suggests that these corals may be useful for δ15N-based paleoceanographic reconstructions. Variability in δ13C values among corals within genera was also low (standard deviation of the mean <±0.5‰) with the exception of Rhipidipathes and Villogorgia. Similar to δ15N, records from the genera studied here with the exception of Rhipidipathes and Villogorgia may be useful for δ13C-based paleoceanographic reconstructions. Overall, using the recommendations developed here, stable isotope records from multiple sites, depths and taxa of these corals can be more rigorously compared. 相似文献
19.
The Lower Cretaceous volcanic formations of Copiapó (Chile) host major stratiform, disseminated, vein, and stockwork mineral
deposits. Among these are the Punta del Cobre district (Cu-Fe) and the neighbouring, large Candelaria deposit (Cu-Fe-Au).
These deposits are likely to have formed during a major extensional event that was accompanied by granitoid emplacement that
triggered important contact metamorphism, metasomatic activity and mineralization processes. We suggest here that alteration-mineralization
processes developed within the upper-plate domain of a NNE-trending, ESE-dipping extensional system, while granitoids were
accomodated within the lower-plate. If this model prove to be right, `Candelaria-type' deposits may be hidden beneath the
present, higher structural position of the Punta del Cobre district.
Received: 13 May 1999 / Accepted: 2 August 1999 相似文献
20.