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  • 206-1256D; Angle of rotation; Bed dip; Bed dip direction; Depth, bottom/max; Depth, reconstructed; Depth, reference; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; Formation microscanner (FMS); Joides Resolution; Leg206; North Pacific Ocean; Ocean Drilling Program; ODP; Piece; Sample code/label; Standard error; Strike; Structure  (1)
  • General Chemistry  (1)
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  • 1
    Electronic Resource
    Electronic Resource
    Weinheim : Wiley-Blackwell
    Berichte der deutschen chemischen Gesellschaft 2000 (2000), S. 1039-1043 
    ISSN: 1434-1948
    Keywords: Iridium ; Amphiphiles ; N ligands ; Structure elucidation ; Chemistry ; General Chemistry
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology
    Notes: The reaction of 4′-functionalized 6′-phenyl-2,2′-bipyridine ligands (L-n) with the dimer [(ppy)2IrCl]2 (ppy = 2-phenylpyridine anion) and subsequent counterion exchange affords a new series of cationic orthometallated iridium(III) complexes, [(ppy)2Ir(L-n)][PF6] (1-5), which have been characterized by spectroscopic methods. These complexes have a large shape anisotropy and significant amphiphilic character. The crystal structure of 4 has been determined by X-ray diffraction.
    Additional Material: 2 Ill.
    Type of Medium: Electronic Resource
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  • 2
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    PANGAEA
    In:  Supplement to: Tartarotti, Paola; Crispini, Laura; Einaudi, Florence; Campari, E (2006): Data report: Reoriented structures in the East Pacific Rise basaltic crust from ODP Hole 1256D, Leg 206: integration of core measurements and electrical-acoustic images. In: Teagle, DAH; Wilson, DS; Acton, GD; Vanko, DA (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 206, 1-26, https://doi.org/10.2973/odp.proc.sr.206.004.2006
    Publication Date: 2024-01-09
    Description: Brittle structures (open fractures and veins) from basaltic oceanic crust drilled at Ocean Drilling Program (ODP) Site 1256 (Guatemala Basin, Pacific Ocean) during Leg 206 were reoriented to the geographic coordinates by (1) correlating structures observed on the core with unoriented images of the exterior of the core and (2) correlating core structures and unoriented images with oriented borehole images. The images of the exterior of the core were obtained by scanning whole-core pieces with the Deutsche Montan Technologie Digital Color Core-Scan system. In the unrolled core images, nonhorizontal planar structures (e.g., veins, faults, or fractures) produce sinusoidal-shaped curves. These can be matched to similar-shaped features imaged along the borehole wall. The borehole images were obtained by the Formation MicroScanner (FMS)-sonic (Dipole Sonic Imager) tool string and the Ultrasonic Borehole Imager (UBI). The FMS provides high-resolution electrical resistivity-based images of borehole walls. FMS images are oriented to magnetic north using the General Purpose Inclinometer Tool. This allows the dip and azimuth of geological features intersecting the hole to be measured from the processed FMS image. The UBI features a high-resolution transducer that provides acoustic images of the borehole wall. The UBI was used in hard rocks for the first time in the history of the ODP during Leg 206.
    Keywords: 206-1256D; Angle of rotation; Bed dip; Bed dip direction; Depth, bottom/max; Depth, reconstructed; Depth, reference; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; Formation microscanner (FMS); Joides Resolution; Leg206; North Pacific Ocean; Ocean Drilling Program; ODP; Piece; Sample code/label; Standard error; Strike; Structure
    Type: Dataset
    Format: text/tab-separated-values, 5838 data points
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