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  • 1
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Wen, Tao; Castro, Clara M; Ellis, Brian R; Hall, Chris M; Lohmann, Kyger C (2015): Assessing compositional variability and migration of natural gas in the Antrim Shale in the Michigan Basin using noble gas geochemistry. Chemical Geology, 417, 356-370, https://doi.org/10.1016/j.chemgeo.2015.10.029
    Publication Date: 2023-01-13
    Description: This study uses stable noble gases' (He, Ne, Ar, Kr, Xe) volume fractions and isotopic ratios from Antrim Shale natural gas to assess compositional variability and vertical fluid migration within this reservoir, in addition to distinguishing between the presence of thermogenic versus biogenic methane. R/Ra values, where R is the measured 3He/4He ratio and Ra is the atmospheric value of 1.384 ± 0.013 × 10**- 6, vary from 0.01 to 0.34 suggesting a largely dominant crustal 4He component with minor atmospheric and mantle contributions. Crustal 21Ne, 40Ar and 136Xe contributions are also present but the atmospheric component is largely dominant for these gases. Crustal contributions for 21Ne, 40Ar and 136Xe vary between 1.1% and 12.5%, between 0.7% and 19% and between 0.1% and 2.7%, respectively. A few samples present higher than atmospheric 20Ne/22Ne ratios pointing to the presence of a small mantle Ne component. High horizontal and vertical variability of noble gas signatures in the Antrim Shale are observed. These are mainly due to variable noble gas input from deep brines and, to a smaller extent, variable in-situ production within different layers of the Antrim Shale, in particular, the Lachine and Norwood members. Estimated 4He ages, considering external 4He input for Antrim Shale water, vary between 0.9 ka and 238.2 ka and match well for most samples with the timing of the major Wisconsin glaciation, suggesting that Antrim Shale water was influenced by glaciation-induced recharge. Consistency between measured and predicted 40Ar/36Ar ratios assuming Ar release temperatures 〉= 250 °C supports a thermogenic origin for most of the methane in these samples. This thermogenic methane is likely to originate at greater depths, either from the deeper portion of the Antrim Shale in the central portion of the Michigan Basin or from deeper formations given that the thermal maturity of the Antrim Shale in the study area is rather low.
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 2
    Publication Date: 2023-02-07
    Keywords: Allen Park 9-8; Antrim_Shale-ANT01; Antrim_Shale-ANT02; Antrim_Shale-ANT03; Antrim_Shale-ANT04; Antrim_Shale-ANT05; Antrim_Shale-ANT06; Antrim_Shale-ANT07; Antrim_Shale-ANT08; Antrim_Shale-ANT09; Antrim_Shale-ANT10; Antrim_Shale-ANT11; Antrim_Shale-ANT12; Antrim_Shale-ANT13; Antrim_Shale-ANT14; Antrim_Shale-ANT15; Antrim_Shale-ANT16; Antrim_Shale-ANT17; Bagley 5 D2-5; Bagley -Livingston B2-2; Camp Ten B3-32; Carbon dioxide; Chester East D3-14; DEPTH, sediment/rock; Dover Ridge A1-5 HDL; Event label; Green River C3-26; Hayes 7 C2-7; Livingston A2-21; Mancelona East A2-23; Methane; Michigan, United States; Nitrogen, gas; Sample ID; St. FredericIX B1-26; St. FredericX A3-25; St. Livingston D2-32; State Charlton 4-7; State Custer D1-12; State Elmira D3-7; State Mancelona 3-26
    Type: Dataset
    Format: text/tab-separated-values, 64 data points
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  • 3
    Publication Date: 2023-02-07
    Keywords: Allen Park 9-8; Antrim_Shale-ANT01; Antrim_Shale-ANT02; Antrim_Shale-ANT03; Antrim_Shale-ANT04; Antrim_Shale-ANT05; Antrim_Shale-ANT06; Antrim_Shale-ANT07; Antrim_Shale-ANT08; Antrim_Shale-ANT09; Antrim_Shale-ANT10; Antrim_Shale-ANT11; Antrim_Shale-ANT12; Antrim_Shale-ANT13; Antrim_Shale-ANT14; Antrim_Shale-ANT15; Antrim_Shale-ANT16; Antrim_Shale-ANT17; Argon-40, isotopic volume fraction; Argon-40, standard deviation; Bagley 5 D2-5; Bagley -Livingston B2-2; Camp Ten B3-32; Chester East D3-14; DEPTH, sediment/rock; Dover Ridge A1-5 HDL; Event label; Green River C3-26; Hayes 7 C2-7; Helium-4, isotopic volume fraction; Helium-4, standard deviation; Livingston A2-21; Mancelona East A2-23; Michigan, United States; Neon-21, isotopic volume fraction; Neon-21, standard deviation; Sample ID; St. FredericIX B1-26; St. FredericX A3-25; St. Livingston D2-32; State Charlton 4-7; State Custer D1-12; State Elmira D3-7; State Mancelona 3-26
    Type: Dataset
    Format: text/tab-separated-values, 119 data points
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  • 4
    Publication Date: 2023-02-08
    Keywords: Allen Park 9-8; Antrim_Shale-ANT01; Antrim_Shale-ANT02; Antrim_Shale-ANT03; Antrim_Shale-ANT04; Antrim_Shale-ANT05; Antrim_Shale-ANT06; Antrim_Shale-ANT07; Antrim_Shale-ANT08; Antrim_Shale-ANT09; Antrim_Shale-ANT10; Antrim_Shale-ANT11; Antrim_Shale-ANT12; Antrim_Shale-ANT13; Antrim_Shale-ANT14; Antrim_Shale-ANT15; Antrim_Shale-ANT16; Antrim_Shale-ANT17; Argon-36/Krypton-84; Argon-36/Krypton-84, standard deviation; Argon-40/Argon-36; Argon-40/Argon-36, standard deviation; Bagley 5 D2-5; Bagley -Livingston B2-2; Camp Ten B3-32; Chester East D3-14; DEPTH, sediment/rock; Dover Ridge A1-5 HDL; Event label; Green River C3-26; Hayes 7 C2-7; Helium-4/Neon-20; Livingston A2-21; Mancelona East A2-23; Michigan, United States; Neon-20/Argon-36; Neon-20/Argon-36, standard deviation; Neon-20/Neon-22; Neon-20/Neon-22, standard deviation; Neon-21/Neon-22; Neon-21/Neon-22, standard deviation; Ratio; Sample ID; St. FredericIX B1-26; St. FredericX A3-25; St. Livingston D2-32; Standard deviation; State Charlton 4-7; State Custer D1-12; State Elmira D3-7; State Mancelona 3-26; Xenon-136/Xenon-130; Xenon-136/Xenon-130, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 289 data points
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  • 5
  • 6
    Electronic Resource
    Electronic Resource
    s.l. ; Stafa-Zurich, Switzerland
    Advanced materials research Vol. 33-37 (Mar. 2008), p. 617-622 
    ISSN: 1662-8985
    Source: Scientific.Net: Materials Science & Technology / Trans Tech Publications Archiv 1984-2008
    Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics
    Notes: Two-phase modelling testing was performed to study the shear strength of rock bridges ofjointed rock mass in this paper. The failure process of rock sample containing multiple collinearcracks was observed. Based on theory of fracture mechanics and analytical method, a rock-bridgefailure model was proposed and the expression of shear strength was derived. Comparison ofcalculated shear strength and the model test results was made and they agree well
    Type of Medium: Electronic Resource
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  • 7
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] All mammals produce heparin, a negatively charged glycosaminoglycan that is a major constituent of the secretory granules of mast cells which are found in the peritoneal cavity and most connective tissues. Although heparin is one of the most studied molecules in the body, its physiological ...
    Type of Medium: Electronic Resource
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  • 8
    ISSN: 1365-2958
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology , Medicine
    Notes: Agrobacterium tumefaciens induces tumours on plants by transferring a nucleoprotein complex, the T-complex, from the bacterium to the plant cell. The T-complex consists of a single-stranded DNA (ssDNA) segment, the T-DNA, and VirD2, an endonuclease covalently attached to the 5′ end of the T-DNA. A type IV secretion system encoded by the virB operon and virD4 is required for the entry of the T-complex and VirE2, a ssDNA-binding protein, into plant cells. The VirE1 protein is specifically required for the export of the VirE2 protein, as demonstrated by extracellular complementation and tumour formation. In this report, using a yeast two-hybrid system, we demonstrated that the VirE1 and VirE2 proteins interact and confirmed this interaction by in vitro binding assays. Although VirE2 is a ssDNA-binding protein, addition of ssDNA into the binding buffer did not interfere with the interaction of VirE1 and VirE2. VirE2 also interacts with itself, but the interaction between VirE1 and VirE2 is stronger than the VirE2 self-interaction, as measured in a lacZ reporter gene assay. In addition, the interaction of VirE2 with itself is inhibited by VirE1, indicating that VirE2 binds VirE1 preferentially. Analysis of various virE2 deletions indicated that the VirE1 interaction domain of VirE2 overlaps the VirE2 self-interaction domain. Incubation of extracts from Escherichia coli overexpressing His-VirE1 with the extracts of E. coli overexpressing His-VirE2 increased the yield of His-VirE2 in the soluble fraction. In a similar purified protein solubility assay, His-VirE1 increased the amount of His-VirE2 partitioning into the soluble fraction. In Agrobacterium, VirE2 was undetectable in the soluble protein fraction unless VirE1 was co-expressed. When urea was added to solubilize any large protein aggregates, a low level of VirE2 was detected. These results indicate that VirE1 prevents VirE2 from aggregating, enhances the stability of VirE2 and, perhaps, maintains VirE2 in an export-competent state. Analysis of the deduced amino acid sequence of the VirE1 protein revealed that the VirE1 protein shares a number of properties with molecular chaperones that are involved in the transport of specific proteins into animal and plant cells using type III secretion systems. We suggest that VirE1 functions as a specific molecular chaperone for VirE2, the first such chaperone linked to the presumed type IV secretion system.
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  • 9
    Electronic Resource
    Electronic Resource
    Oxford [u.a.] : International Union of Crystallography (IUCr)
    Acta crystallographica 56 (2000), S. 418-420 
    ISSN: 1600-5759
    Source: Crystallography Journals Online : IUCR Backfile Archive 1948-2001
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Notes: In the title complex, [MnHg(SCN)4(C2H6SO)2]n, each Hg atom is tetrahedrally coordinated to four S atoms of the SCN ions, while each Mn atom is octahedrally coordinated to four N atoms of the SCN ions and two O atoms of the dimethyl sulfoxide molecules which occupy the trans positions. Each pair of Hg and Mn atoms is bridged by one SCN ion. Two Mn atoms, two Hg atoms and four SCN ions make a 16-membered ring which organises into a two-dimensional network. The dimethyl sulfoxide ligands are extended perpendicular to the plane on both sides.
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  • 10
    Electronic Resource
    Electronic Resource
    Oxford [u.a.] : International Union of Crystallography (IUCr)
    Acta crystallographica 56 (2000), S. e172-e173 
    ISSN: 1600-5759
    Source: Crystallography Journals Online : IUCR Backfile Archive 1948-2001
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Notes: The title compound, [Re2O3(C19H20N2O2)2], is a hexacoordinate complex containing an [Re2O3]4+ core with a linear O=Re—O—Re=O bridge. The distorted octahedral coordination of the ReV atom is achieved by an N2O2 donor set from the tetradentate imine–phenol ligand. The overall charge of the compound is neutral due to deprotonation of the phenol groups, and the terminating and bridging O atoms. The Re=O and Re—O bond distances of the [Re2O3]4+ core are 1.699 (4) and 1.911 (1) Å, respectively. The Re—O and Re—N bond distances of the equatorial plane are in the ranges 2.024 (4)–2.013 (4) and 2.128 (5)–2.120 (5) Å, respectively.
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