E‐learning: new opportunities in continuing professional development
The growth in professional learning is opening up many new opportunities for the application of e‐learning to the world of continuing professional development (CPD). CPD programmes require professionals to engage in annual programmes of professional development, and in some cases revalidation or recertification. To date, most of this activity has been off‐line. Increasingly, CPD requirements will be satisfied through the use of learning resources available on‐line or packaged into specially tailored e‐learning courses. Societies and professional associations – as the primary managers and coordinators of CPD programmes – are in a strong position to expand upon their existing Web‐based initiatives to deliver a new generation of e‐learning services to their members.
Evaluating online CPD using educational criteria derived from the experiential learning cycle
A set of educational evaluation criteria for online continuing professional development (CPD) courses is developed using Kolb’s (1984) experiential learning cycle theory. These criteria are used to evaluate five courses provided by online CPD websites. It was found that these online CPD courses neglect parts of the learning cycle. Suggestions for improvements in these areas are given.
Mississippian Barnett Shale: Lithofacies and depositional setting of a deep-water shale-gas succession in the Fort Worth Basin, Texas
The Mississippian Barnett Formation of the Fort Worth Basin is a classic shale-gas system in which the rock is the source, reservoir, and seal. Barnett strata were deposited in a deeper water foreland basin that had poor circulation with the open ocean. For most of the basin's history, bottom waters were euxinic, preserving organic matter and, thus, creating a rich source rock, along with abundant framboidal pyrite. The Barnett interval comprises a variety of facies but is dominated by fine-grained (clay- to silt-size) particles. Three general lithofacies are recognized on the basis of mineralogy, fabric, biota, and texture: (1) laminated siliceous mudstone; (2) laminated argillaceous lime mudstone (marl); and (3) skeletal, argillaceous lime packstone. Each facies contains abundant pyrite and phosphate (apatite), which are especially common at hardgrounds. Carbonate concretions, a product of early diagenesis, are also common. The entire Barnett biota is composed of debris transported to the basin from the shelf or upper oxygenated slope by hemipelagic mud plumes, dilute turbidites, and debris flows. Biogenic sediment was also sourced from the shallower, better oxygenated water column. Barnett deposition is estimated to have occurred over a 25-m.y. period, and despite the variations in sublithofacies, sedimentation style remained remarkably similar throughout this span of time.