By M. Church, Mario Coniglio, L. A. Hardie, F. J. Longstaffe, V. Middleton
This finished, one-volume encyclopedia covers the sedimentological features of sediments and sedimentary rocks. It good points greater than 250 entries by way of a few a hundred and eighty eminent individuals from world wide, very good indices, pass references, and large bibliographies.
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This accomplished, one-volume encyclopedia covers the sedimentological facets of sediments and sedimentary rocks. It good points greater than 250 entries via a few a hundred and eighty eminent participants from worldwide, first-class indices, go references, and huge bibliographies.
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Extra info for Encyclopedia of Sediments & Sedimentary Rocks
A. and Spearing, P. ). Sandstone Depositional Environments. Memoir: American Association of Petroleum Geologists 31: pp. 49-86. , 1984. Bibliography of Alluvial-fan Deposits. Norwich: Geobooks, 96p. , and Church, M. ), 1990. Alluvial Fans: A Field Approach. Chichester: Wiley, 391 p. , 1973. Depositionalsedimetitary environments with reference to terrigenous classics. , Berlin: Springer Verlag, 1983. 549p. , 1986. Alluvial fan development and the glacio-glaciofluvial cycle, Nemana Valley, Alaska.
Alluvial sedimentation. International Association of Sedimentologists, Special Publication 17, pp. 235-276. , 1982. Alluvial fan deposits. A. and Spearing, P. ). Sandstone Depositional Environments. Memoir: American Association of Petroleum Geologists 31: pp. 49-86. , 1984. Bibliography of Alluvial-fan Deposits. Norwich: Geobooks, 96p. , and Church, M. ), 1990. Alluvial Fans: A Field Approach. Chichester: Wiley, 391 p. , 1973. Depositionalsedimetitary environments with reference to terrigenous classics.
However, will cap a succession of rocks that display a variety of subsurface karst features. By comparison, a hardground will be found in a succession of marine sediments that display no evidence of diagenesis in a karst setting. Open and filled cavities Open and filled cavities, whieh range in size from micropores to large caves, are eommon features in many aneient karst terrains. Sueh cavities may have formed through the selective dissolution of metastable mineral components in heterogeneous 13 carbonates whereas others are independent of fabric.