Hand receipt covering contents of components of end items (COEI), basic issue items (BII), and additional authorization list (AAL) for truck, cargo, 1 1/4 ton, 4 x 4, M880 (2320-00-579-8942)...; truck, cargo, 1 1/4 ton, 4 x 2, M890 (2320-00-579-8991)...; truck, ambulance, 1 1/4 ton, 4 x 2, M886 (2310-00-579-9078); truck, ambulance, 1 1/4 ton, 4 x 4, M893 (2310-00-125-5679); truck, telephone maintenance, tactical, 1 1/4 ton, 4 x 4, M888 (2320-01-044-0333).

"May 1983."

Die erdollagerstatten und ubrigen kohlenwasserstoffvorkommen der erdrinde. Grundlagen der petroleum geologie. Mit 125 textabbildungen und 40 tabellen

Mode of access: Internet.

To investigate the causes of the decline of cotton prices. Hearings, Seventy-fourth Congress, second session, pursuant to S. Res. 103, 125, 172, and 182,

pt.1. February 17 to March 31, 1936. 824 p.--pt.2. April 1 to 30, 1936. pp. 825-1524.

Saadja Al-fajjûmi's arabische Psalmenübersetzung und Commentar (Psalm 125-150)

vorgelegt von Bernhard Schreier aus Drohobycz

(Table 1) Organic acid analyses from ODP Leg 125 interstitial waters

For the first time, short-chain organic acids are described from serpentine-associated interstitial waters. In this geologic setting, formate typically dominates the organic acid assemblage. Within the forearc setting, the organic acids are associated only with unconsolidated serpentine. Their existence may be the result of alkaline hydrolysis of ester linkages in organic matter that has been entrained in the serpentine diapir.

(Table 1) Strontium isotopic ratios of interstitial waters from ODP Leg 125 holes

The strontium isotopic data presented here are from interstitial waters squeezed from unconsolidated serpentine, an unusual type of substrate that was recovered from Mariana and Bonin forearc seamounts and has not been previously drilled by the Deep Sea Drilling Project or Ocean Drilling Program. The texture and composition of some of these serpentine deposits from Conical Seamount, located on the Mariana forearc, indicate emplacement as low- or high-viscosity, cold gravitational flows, which are therefore neither sediment nor igneous rock. The strontium isotopic ratios of the interstitial waters from the unconsolidated serpentine range from 0.70912 to 0.70525 and trend toward a relatively less radiogenic composition with increasing sub-bottom depth. These strontium isotopic ratios are derived from at least two strontium sources: seawater and igneous. The strontium isotopic gradients from the interstitial waters from the Leg 125 sites are probably the result of diffusive transport of strontium from an igneous source deep within the lithosphere that may be contaminated with subducted or underplated sediment.