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Guo XuequanSoutheast Hubei Geological Party Hubei Bureau of Geology Mineral Resources Daye Hubei 《《地质学报》英文版》1994,68(3)
This paper discusses geological-geophysical-geochemical models of such typical deposits as the Tieshan-type Fe-Cu deposit, the Tonglushan-type Cu-Fe deposit, the Yehuaxiang-type Cu deposit, the Jiguanzui-type Cu-Au deposit, and the Tongshankou-type Cu (Mo) deposit. The models were established based on practical data of the polymetallic deposits dominated by copper ore in southeastern Hubei. These models, which are graphically illustrated in the paper, systematically summarize the metallogenic geological conditions and the geophysical-geochemical characteristics of copper deposits in this area. The models are of practical significance for studying copper deposits, predicting mineral resources, choosing exploration methods, and searching for ore deposits based on existing ones in the study area. 相似文献
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Single crystalline San Carlos olivine (1 mm cube) was transformed to (Mg,Fe)2SiO4β-phase at 13.5–15 GPa, 1030–1330 °C for 0–600 min using a multi-anvil high pressure apparatus. The α-β transformation occurred
by incoherent surface nucleation and interface-controlled growth and recovered partially transformed samples showed sharply
defined reaction rim. The growth rate of the β-phase rim significantly decreased with time and the growth eventually ceased.
TEM observations revealed that many dislocations were created in both the relict olivine just near the α-β interface and the
β-phase in the rim, which show evidence for deformation caused by interfacial stresses associated with the misfit elastic
strain of the transformation. The observed tangled dislocation texture in β-phase suggested that the β-phase rim was hardened
and relaxation of the interfacial stress was retarded. This probably caused a localized pressure drop in the relict olivine
and decreased the growth rate. Time-dependent growth rates of β-phase is possibly controlled by the rheology of β-phase, which
must be considered for the prediction of the olivine metastability in the subducting slabs.
Received: 24 January 1997 / Revised, accepted: 24 July 1998 相似文献
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Please?refer?to?the?attachment(s)?for?more?details. 相似文献
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P. F. Zanazzi P. Comodi S. Nazzareni N. Rotiroti S. van Smaalen 《Physics and Chemistry of Minerals》2007,34(1):23-29
The thermal evolution of 10-Å phase Mg3Si4O10(OH)2·H2O, a phyllosilicate which may have an important role in the storage/release of water in subducting slabs, was studied by X-ray single-crystal diffraction in the temperature range 116–293 K. The lattice parameters were measured at several intervals both on cooling and heating. The structural model was refined with intensity data collected at 116 K and compared to the model refined at room temperature. As expected for a layer silicate on cooling in this temperature range, the a and b lattice parameters undergo a small linear decrease, α a = 1.7(4) 10?6 K?1 and α b = 1.9(4) 10?6 K?1, where α is the linear thermal expansion coefficient. The greater variation is along the c axis and can be modeled with the second order polynomial c T = c 293(1 + 6.7(4)10?5 K?1ΔT + 9.5(2.5)10?8 K?2(ΔT)2) where ΔT = T ? 293 K; the monoclinic angle β slightly increased. The cell volume thermal expansion can be modeled with the polynomial V T = V 293 (1 + 8.0 10?5 K?1 ΔT + 1.4 10?7 K?2 (ΔT)2) where ΔT = T ? 293 is in K and V in Å3. These variations were similar to those expected for a pressure increase, indicating that T and P effects are approximately inverse. The least-squares refinement with intensity data measured at 116 K shows that the volume of the SiO4 tetrahedra does not change significantly, whereas the volume of the Mg octahedra slightly decreases. To adjust for the increased misfit between the tetrahedral and octahedral sheets, the tetrahedral rotation angle α changes from 0.58° to 1.38°, increasing the ditrigonalization of the silicate sheet. This deformation has implications on the H-bonds between the water molecule and the basal oxygen atoms. Furthermore, the highly anisotropic thermal ellipsoid of the H2O oxygen indicates positional disorder, similar to the disorder observed at room temperature. The low-temperature results support the hypothesis that the disorder is static. It can be modeled with a splitting of the interlayer oxygen site with a statistical distribution of the H2O molecules into two positions, 0.6 Å apart. The resulting shortest Obas–OW distances are 2.97 Å, with a significant shortening with respect to the value at room temperature. The low-temperature behavior of the H-bond system is consistent with that hypothesized at high pressure on the basis of the Raman spectra evolution with P. 相似文献
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Based on the established mathematic model and graphic interpretation, a new method, which is used to calculate the contribution of single-zone production in a commingled producing well by the ultraviolet spectrum technique, has been established. The standard plate was drawn using the extinction coefficient E of sample oils formulated artificially as y-axis and the wavelength as x-axis. The curve resulting from the UV analysis of sample oils in the commingled well was inserted into the standard plate and compared. The proportion of each single zone in the commingled producing well was identical with the proportion of the curve which is closest to the curve of sample oils formulated artificially. In the well QHD32-6-3 field, taking well A22 for example and using this method, the production contribution of a single zone was calculated. The result showed that the Nm4 zone is a major "contributor", the proportion of the Nm4 zone is 70%, and that of the Nm1 zone is 30%. The ultraviolet spectrum technique provided a new reservoir geochemical technique of monitoring production contribution, especially for biodegraded heavy oil, but it has some limitation, just depending on the GC fingerprint technique. 相似文献
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Sandstones of Punagarh basin of Trans Aravalli region, NW Indian shield were analyzed for their major and trace element contents in conjunction with petrographic modes. The Punagarh basin comprises four formations (Sojat, Bambolai, Khamal and Sowania), amongst which the Sojat Formation in uncoformable contact with overlying formations, is significantly older and enjoys separate status as rest of the formations constitute Punagarh Group. Petrographic attributes suggest that Sojat sandstones contain distinct modal abundances like high content of quartz and low content of feldspar, mica, matrix, rock fragments and cement. In general there is a decrease in the average modal abundance of quartz and mica with concomitant increase of feldspar, chert and rock fragments from base to top in Punagarh sandstones. Sojat sandstones are also geochemically distinct as they possess high SiO2/Al2O3, Th/U and Cr/Th ratios coupled with lowest Na2O/K2O ratio and Zr content, least fractionated LREE, more fractionated HREE and largest Eu* anomaly compared to Punagarh sandstones. The weathering indices suggest intense chemical weathering for Sojat sandstones and low to moderate for Punagarh sandstones. Compositionally all the sandstones of the Punagarh basin come under the category of quartzarenite. Compared to PAAS and UCC, both suite of sandstones are generally depleted in REE, HFSE (with exception of Zr, Hf and Ta), and enriched in ferromagnesian trace elements particularly Cr and Co. The chemical data indicate that the sediments were derived from the source(s) of mixed felsic - mafic composition, with the former being dominant. The source rocks were granites, TTG, basalts, and rhyolites. The Sojat sandstones owe their source form Archean crust while Punagarh sandstones got detritus from Mesoproterozic crust. Immobile element ratios and REE abundances of Sojat sandstones closely match with Paleoproterozoic metagreywackes of Ghana of African craton while Punagarh sandstones show near geochemical characteristic with Gogunda, Kumbalgarh and Vindhyan quartzites of Aravalli craton. This geochemical similarity of Sojat sandstones provides credence to the hypothesis that Trans–Aravalli region of India had been an integral part of Arabian - Nubian shield. The chemical data advocate the deposition of these sandstones in a tectonic setting comparable to modern back arc setting. 相似文献
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Qian JianxingThe Second Institute of Oceanography SO A Hangzhuu Zhejiang Liu Linqun 《《地质学报》英文版》1995,69(2)
Based on a comparison between the oxygen isotope records of benthic and plank tonic foraminifers from core 8KL of the South China Sea and sea-level change records derived from the Huon Peninsula, New Guinea, it is found that both records are very similar from 72 K a B.P. to the present, especially for the benthic oxygen isotope record. The linear regression shows that δ18O changes (0.9995‰ for benthic foraminifers and 1.022‰ for planktonic foraminifers) are equal to 100 m in sea-level fluctuation. After making temperature correction in the δ18O record of benthic foraminifers from 72 to 120 Ka B.P., the curve of sea-level oscillation of the South China Sea since 186 Ka B.P. has been reconstructed. The lowermost sea - level that occurred in the last glacial maximum and oxygen isotope stage 6 is approximately - 130 m. 相似文献
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Please?refer?to?the?attachment(s)?for?more?details. 相似文献
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Liu Zhili Liu Xuexian Li Pengfu Department of Biology Nanjing University Nanjing Jiangsuand Du Rulin Hebei College of Geology Shijiazhuang Hebei Fei Zhenbi 《《地质学报》英文版》1995,69(4):387-395
The authors studied the biomarkers (alkanes) of eight iron ore samples from Nianpanshan and Dsbaodui of Pangjiabao and Longguan, Xuanhua, Hebei. These samples have higher nC15-nC20 contents, with main peaks at nC16, nC 17 and nC18, and contain abundant pristane and phytane. These results indicate that iron stromatolite and iron oncolites in orebodies are sedimentary structures of algal origin. Sedimentary iron accumulation mainly results from activity of blue algae. This study provides new valuable evidence for the origin of Xuanlong-type iron deposits. 相似文献
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《中国地球化学学报》2004,(4)
No .1Mantle/CrustEvolutionandEco EnvironmentalEffectsasExemplifiedbyZhangjiakou WestBeijingRegion NIUShuyinetal.(1)…………………………………………………………………………………OrganicPetrologicalStudiesonImmatureSourceRocks LIXianqingetal .(15 )…………………………………ChemistryofAerosolsoverChukchiSeaandBeringSea ZHULaiminetal .(2 6 )…………………………………TemporalandSpatialDistributionofElementsinaSmallCatchment ,andBufferFunctionofWetlandinLongganLake ,China WUYanhong… 相似文献
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《中国地质大学学报(英文版)》2001,12(2)
Ｎｏ .1ＰｒｏｖｅｎａｎｃｅｏｆＰａｌｅｏｇｅｎｅｓｅｄｉｍｅｎｔｓｉｎＨｏｈＸｉｌｂａｓｉｎ ,ｎｏｒｔｈｏｆＱｉｎｇｚａｎｇｐｌａｔｅａｕ ,ａｎｄｉｔｓｓｉｇｎｉｆｉｃａｎｃｅｆｏｒ ｐｌａｔｅａｕｕｐｌｉｆｔ.ＬｉｕＺｈｉｆｅｉ,ＷａｎｇＣｈｅｎｇｓｈａｎ ,ＹｉＨａｉｓｈｅｎｇａｎｄＬｉｕＳｈｕｎ .(1) :1- 6 .ＴｈｅＨｏｈＸｉｌｂａｓｉｎ ,ｔｈｅｌａｒｇｅｓｔＴｅｒｔｉａｒｙｓｅｄｉｍｅｎｔａｒｙｂａｓｉｎｉｎｔｈｅｈｉｎｔｅｒｌａｎｄｏｆｔｈｅＱｉｎｇｚａｎｇｐｌａｔｅａｕｂｅｔｗｅｅｎｔｈｅ… 相似文献
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A continuous Ordovician-Silurian boundary section from the upper Wufeng Formation through the Kuanyinchiao Formation to the lower Lungmachi Formation has been carefully measured and collected at Shuanghe of Changning, southern Sichuan Province. For the first time, the temporal changes of α- and β-diversities of the Hirnantia fauna have been discussed in great detail. The general trend of brachiopod diversity change, increasing upward, is consistent with the regional trend of the Yangtze Platform, which had been controlled by both intrinsic and extrinsic factors. However, the sudden drop of diversity for a short period in the upper Kuanyinchiao Formation might have been controlled by environmental factors rather than normal faunal turnover. Synecological analysis using numerical methods recognizes two brachiopod-dominated associations of the Hirnantia fauna, the Dalmanella-Kinnella Association and the Mirorthis Association, both living in an offshore, deeper water environment corresponding to BA3-upper BA4, particularly lower BA3. 相似文献