Ancient Sedimentary Environments: And Their Sub-Surface - download pdf or read online
By Selley Richard C.
This variation keeps the case historical past method of emphasize the subsurface analysis of environments utilizing seismic and geophysical good logs and their software to petroleum exploration and creation. This booklet will be of curiosity to undergraduates in sedimentology and petroleum geology.
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Additional info for Ancient Sedimentary Environments: And Their Sub-Surface Diagnosis
The second problem, that of deducing the habitat of a fossil, is also a very real one which has been discussed extensively in the literature. To consider one simple case, it has been pointed out that bears live today from the arctic to the equator. 4). Lest the preceding paragraphs have painted too gloomy a picture of fossils as environmental indicators it must be stated that they are one of the most valuable techniques available. Of all the different fossils that can be used in environmental analysis perhaps two ofthe most important types are micro-fossils and trace fossils.
Lest the preceding paragraphs have painted too gloomy a picture of fossils as environmental indicators it must be stated that they are one of the most valuable techniques available. Of all the different fossils that can be used in environmental analysis perhaps two ofthe most important types are micro-fossils and trace fossils. Micro-fossils have the great advantage over mega-fossils that they are recoverable from well cuttings, and that a small volume of rock may contain sufficient specimens to be used in statistical studies.
Second, it has been noted that certain types of trace characterize particular environments, though the beasts responsible may be unknown. Using this fact workers have defined a series of ' ichnofacies'. Each ichnofacies consists of a suite of trace fossils which occur in characteristic sedimentary facies whose environment may be determined independently (see Seilacher, 1967; Rodriguez and Gutschick, 1970; and Heckel, 1972). These ichnofacies have remained constant through Phanerozoic time, despite the evolution of the creatures responsible (Fig.
Ancient Sedimentary Environments: And Their Sub-Surface Diagnosis by Selley Richard C.