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88 Ga) of the Wopmay Orogen this arc terrane collided with the Slave craton, causing compression, shortening, and the eastward translation of exotic material (Fig 1115c) In the seismic pro le (Fig 1115b), the accreted Proterozoic crust displays gently folded upper crustal layers overlying re ectors that appear to be thrust slices above detachment faults that atten downward into the Moho Remnants of the old, east-dipping subduction zone associated with the collision are still visible today as re ections that project to 200 km or more beneath the Slave craton Once accretion of the Hottah terrane terminated, the subduction of oceanic lithosphere to the east beneath the continental margin created the 188 184 Ga Great Bear Magmatic arc and eventually led.

produced a zone of extremely thin continental crust This thin crust is characterized by tilted fault blocks that are underlain by a prominent subhorizontal re ector (S) that probably represents a serpentinized shear zone at the crust mantle boundary (Fig 734c) (Reston et al, 1996) The re ector occurs seaward of stretched continental basement and above a high velocity lower layer of serpentinized mantle Below the re ector seismic velocities increase gradually with depth and approach normal mantle velocities at depths of 15 20 km Seaward of the thinned continental crust and landward of the rst oceanic crust, a transitional region is characterized by low basement velocities, little re ectivity, and a lower layer of serpentinized mantle showing velocities (Vp > 70 km s 1) that are similar to high velocity lower crust.

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An accountant can have the finest costing system in the world and still waste time recording inventory transactions if the record accuracy level of those transactions is poor. Because the accounting department is often held responsible if recorded inventory costs are wrong, one should have a clear idea of how to set up an inventory tracking system, conduct physical inventory counts, and cycle count inventory on an ongoing basis in order to have greater confidence in the inventory record accuracy. Although the accountant may not have control over these systems, it is helpful to know how they should be run. It is also increasingly common for controllers to be given management-level control over the warehouse solely because they will then have central and undisputed responsibility for inventory record accuracy. This chapter notes several counting policies that management should approve and support, as well as procedures for setting up inventory tracking systems, conducting physical inventory counts, ensuring a proper inventory cutoff, reconciling inventory variances, running successful cycle counting programs, and reducing the need for inventory tracking.

Farther seaward, the basement is characterized by a complex series of peridotite ridges (PR), which contain sea oor spreading magnetic anomalies that approximately parallel the strike of the oceanic spreading center Although this zone is composed mostly of serpentinized mantle, it may also contain minor intrusions Thus, basement at these margins consists of faulted continental blocks, a smooth transitional region, and elevated highs Moho re ections (M) are absent within the ocean continent transition zone Instead, this region displays landward and seaward dipping re ectors that extend to depths of 15 20 km In the second type of nonvolcanic margin (Fig 734d), based primarily on the Labrador example, only one or two tilted fault blocks of upper continental crust are observed and the S-type horizontal re ection is absent A zone of thinned mid-lower continental crust occurs beneath a thick sedimentary basin.

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A transitional region occurs farther seaward in a manner similar to the section shown in Fig 734c However, dipping re ections within the upper mantle are less prevalent For Labrador, the region of extended lower continental crust is very wide with a thick sedimentary basin, while for Flemish Cap and the Newfoundland basin, the width of extended lower continental crust is narrow or absent Moho re ections (M) indicate very thin ( 5 km) oceanic crust..

June 12, 2004

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