Die Meisterwerke der Königl. Gemälde-Galerie zu Cassel : 209 Kunstdrucke nach den Originalgemälden /

Mode of access: Internet.

Kantate Nr. 209. [music] : Non sa che sia dolore = Was Schmerz sei und was Leiden : BWV 209 /

For Soprano solo.

Finance docket no. 1176 : maintenance expenses under section 209.

"Submitted December 4, 1920. Decided July 12, 1921."

The register of Thomas de Cantilupe, Bishop of Hereford (A.D. 1275-1282) /

Includes index.

Operator and organizational maintenance manual : truck, lift, fork, GED, solid rubber tired wheels, 4000 lbs capacity, 180 in lift, Army model MHE 209, Allis Chalmers model F40-24PS, FSN 3930-459-5948.

"August 1970."

Field and depot maintenance manual : engine, gasoline, fuel injected, supercharged, horizontal-opposed, air cooled, six cylinder, assembly-2805-528-6015, (Continental model AOSI-895-5 and AOSI-895-5M) : end item application : gun, self-propelled, full tracked, twin 40-mm, M42A1 (TM 9-2350-202), howitzer, self-propelled, full tracked, 105-mm, M52A1 (TM 9-2350-209) ....

Includes index.

Direct support and general support maintenance repair parts and special tools lists (including depot maintenance repair parts and special tools lists) : truck, lift, fork, GED; solid rubber tired wheels, 4000 lb capacity, 180 in lift, Army model MHE 209, NSN 3930-00-459-5948, Allis-Chalmers model F40-24PS and 100 in lift, Army model MHE 224, NSN 3930-00-165-4102, Allis-Chalmers model F40-24PS100.

Includes index.

Chemical and isotopic composition of carbonate veins from ODP Leg 209

Carbonate veins hosted in ultramafic basement drilled at two sites in the Mid Atlantic Ridge 15°N area record two different stages of fluid-basement interaction. A first generation of carbonate veins consists of calcite and dolomite that formed syn- to postkinematically in tremolite-chlorite schists and serpentine schists that represent gently dipping large-offset faults. These veins formed at temperatures between 90 and 170 °C (oxygen isotope thermometry) and from fluids that show intense exchange of Sr and Li with the basement (87Sr/86Sr = 0.70387 to 0.70641, d7Li L-SVEC = + 3.3 to + 8.6 per mil). Carbon isotopic compositions range to high d13C PDB values (+ 8.7 per mil), indicating that methanogenesis took place at depth. The Sr-Li-C isotopic composition suggests temperatures of fluid-rock interaction that are much higher (T > 350-400 °C) than the temperatures of vein mineral precipitation inferred from oxygen isotopes. A possible explanation for this discrepancy is that fluids cooled conductively during upflow within the presumed detachment fault. Aragonite veins were formed during the last 130 kyrs at low-temperatures within the uplifted serpentinized peridotites. Chemical and isotopic data suggest that the aragonites precipitated from cold seawater, which underwent overall little exchange with the basement. Oxygen isotope compositions indicate an increase in formation temperature of the veins by 8-12 °C within the uppermost ~ 80 m of the subseafloor. This increase corresponds to a high regional geothermal gradient of 100-150 °C/km, characteristic of young lithosphere undergoing rapid uplift.