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  • Inorganic Chemistry  (3)
  • 22-214; 22-215; 22-216; Caesium; Cerium; Chromium; Copper; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Emission spectrometry; Europium; Event label; Glomar Challenger; Indian Ocean//BASIN; Indian Ocean//RIDGE; Lanthanum; Lanthanum/Samarium ratio; Lanthanum/Ytterbium ratio; Leg22; Nickel; Potassium; Potassium/Caesium ratio; Potassium/Rubidium ratio; Rock type; Rubidium; Samarium; Sample code/label; Strontium-87/Strontium-86 ratio; Terbium; Vanadium; Ytterbium  (1)
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  • 1
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    PANGAEA
    In:  Supplement to: Reddy, V Viswanatha; Subbarao, K V; Reddy, G R; Matsuda, J; Hekinian, Roger (1978): Geochemistry of volcanics from the Ninetyeast Ridge and its vicinity in the Indian Ocean. Marine Geology, 26(1-2), 99-117, https://doi.org/10.1016/0025-3227(78)90048-8
    Publication Date: 2023-06-27
    Description: The basalts and oceanic andesites from the aseismic Ninetyeast Ridge display trachytic, vesicular and amygdaloidal textures suggesting a subaerial volcanic environment. The normative composition of the Ninetyeast Ridge ranges from olivine picriteto nepheline-normative alkaline basalt, suggesting a wide range of differentiation. This is further supported by the fractionation-differentiation trends displayed by transition metal trace elements (Ni, Cr, V and Cu). The Ninetyeast Ridge rocks are enriched in rare earth (RE) and large ion lithophile (LIL) elements and Sr isotopes (0.7043-0.7049), similar to alkali basalts and tholeiites from seamounts and islands, but different from LIL-element-depleted tholeiitic volcanic rocks of the recent seismic mid-Indian oceanic ridge. The constancy of 87Sr/86Sr ratios for basalts and andesites is compatible with a model involving fractional crystallization of mafic magma. The variation of 87Sr/86Sr ratios between 0.97 and 2.79 may possibly be explained in terms of a primordial hot mantle and/or chemically contrasting heterogeneous mantle source layers relatively undepleted in LIL elements at different periods in the geologic past. In general, the Sr isotopic data for rocks from different tectonic environments are consistent with a "zoning-depletion model" with systematically arranged alternate alkali-poor and alkali-rich layers in the mantle beneath the Indian Ocean.
    Keywords: 22-214; 22-215; 22-216; Caesium; Cerium; Chromium; Copper; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Emission spectrometry; Europium; Event label; Glomar Challenger; Indian Ocean//BASIN; Indian Ocean//RIDGE; Lanthanum; Lanthanum/Samarium ratio; Lanthanum/Ytterbium ratio; Leg22; Nickel; Potassium; Potassium/Caesium ratio; Potassium/Rubidium ratio; Rock type; Rubidium; Samarium; Sample code/label; Strontium-87/Strontium-86 ratio; Terbium; Vanadium; Ytterbium
    Type: Dataset
    Format: text/tab-separated-values, 158 data points
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  • 2
    ISSN: 0009-2940
    Keywords: Cyclophosphahydrazides ; Dinitrogen-bridged ; Conformation ; Chair and Boat forms ; Dinuclear Mo(0) complexes ; 1,2,4,5,3,6-Tetrazadiphosphorinanes ; Chemistry ; Inorganic Chemistry
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology
    Notes: The reactions of methylhydrazine with RPC12 (R = Et, tBu, and Ph) produced the cyclic phosphorus (III) hydrazides (1,2,4,5,3,6-tetrazadiphosphorinanes) [RPN(Me)N(H)2 (R = Et, 1; (Ph, 2; tBu, 3) in good yields. The 1H-and 31P-NMR spectroscopic analysis indicated that 1 exists in chair and boat conformations. However, it crystallizes in the chair conformation exclusively. The X-ray crystallographic investigation of all the three cyclo-phosphorus hydrazides 1-3 confirms the existence of these compounds in the chair conformations in the solid state. The reaction of Mo(CO)4-(NHC5H10)2 with 1 and 2 gives the dinuclear Mo(0) complexes [{Mo(CO)4(NHC5H10)}2(μ-[RPN(Me)N(H)]2}] (R = Et, 5; Ph, 6). Based on 1H- and 31P-NMR spectroscopic data, a bridging dinuclear dimetallic formulation is proposed for 5 and 6. The IR spectra indicate that the carbonyls are disposed in cis-geometry around the Mo(0) center.
    Additional Material: 6 Ill.
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  • 3
    Electronic Resource
    Electronic Resource
    Weinheim : Wiley-Blackwell
    Berichte der deutschen chemischen Gesellschaft 127 (1994), S. 1355-1357 
    ISSN: 0009-2940
    Keywords: Diphosphanylhydrazides ; Diphosphanes, dinitrogen-bridged ; Cycloplatinaphosphahydrazides ; Chemistry ; Inorganic Chemistry
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology
    Notes: While the transition metal complexes of bis(phosphanyl)amines (PII-N-PIII) have been known for over three decades, the ligating properties of the next homologue PIII-N-N-PIII have been unprecedented so far. The X-ray structures of cycloplatinaphosphanehydrazides, [(OR)2PN(Me)N(Me)P(OR)2-PtCl2], reveal short distances for the P-N [1.639(5) Å] bonds.
    Additional Material: 2 Ill.
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  • 4
    ISSN: 0044-2313
    Keywords: Phosphanyl Hydrazide ; Phosphinoamine ; Triphosphine ; Trimetallic Complexes ; Chemistry ; Inorganic Chemistry
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology
    Description / Table of Contents: Übergangsmetall-Chemie von Hydraziden der Hauptgruppen-Elemente. 17 Triphosphan aus Phosphanylhydrazid als Baustein für Heterotrimetall-Verbindungen. Synthese und Koordinationschemie von (Me2P)2N—N(Me)(PMe2)Das neue Triphosphan (Me2P)2N—N(Me)(PMe2) (1) ist in reiner Form durch Reaktion von Methylhydrazin mit Dimethylchlorphosphan in Gegenwart von Triethylamin dargestellt worden. Dieses Triphosphan stellt eine Brücke zwischen dem Phosphinoamin (〉P—N(R)—P〈) und dem Phosphanylhydrazid (〉P—N(R)—N(R)—P〈) dar. Die Reaktion von 1 mit cis-[W(CO)4(NHC5H10)2] erfolgt über zwei Koordinationswege zu viergliedrigen M—P—N—P und fünfgliedrigen M—P—N—N—P Metallazyklen. Der Wolframkomplex cis-[W(CO)4{(Me2P)2NN(Me)(PMe2)}] (2) hat eine unkoordinierte Phosphangruppe über die Organomultimetall-Verbindungen erhalten werden können. Zum Beispiel ergibt die Reaktion von 2 mit PdCl2(PhCN)2 und PtCl2(COD) die trimetallischen Komplexe mit W0—PtII- und W0—PdII-Zentren in relativ guten Ausbeuten. Die verschiedenen Isomeren dieser dreikernigen Komplexe wurden durch 31P-NMR-Spektroskopie identifiziert.
    Notes: The new triphosphine (Me2P)2N—N(Me)(PMe2) (1), has been synthesized in pure form by the reaction of methylhydrazine with dimethylchlorophosphine in the presence of triethylamine. This triphosphine represents a bridge between phosphinoamine (〉P—N(R)—P〈) and phosphanyl hydrazide (〉P—N(R)—N(R)—P〈) backbones. Reaction of 1 with cis-[W(CO)4(NHC5H10)2] proceeds via two coordination modes to give four-membered M—P—N—P and five-membered M—P—N—N—P metallacyclic frameworks. The tungsten complex cis-[W(CO)4{(Me2P)2NN(Me)(PMe2)}] (2) possessing an uncoordinated phosphine moiety to prepare multimetallic organometallic compounds. For example, reactions of 2 with PdCl2(PhCN)2 and PtCl2(COD) produced the trimetallic complexes consisting of W(0)—Pt(II) and W(0)—Pd(II) centers respectively in good yields. The different isomers of these trinuclear complexes have been clearly identified by 31P NMR spectroscopy.
    Additional Material: 1 Ill.
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