. Bulletin of the Geological Society of America. Geology. STRUCTURE 295 The means by which these several structural features are determined may be here pointed out. Such a statement will also serve to explain why only the major structural relations are determinable. CALCAREOUS Kp^ SLATE SERIES. LEGEND Cono/omer<9te Figure 1.—Sketch Map showing Pre-Cambrian Structure in northern Blaok Hills Within this series of schists there are only a few stratigraphic mem- bers which are sufficiently persistent and distinctive to permit tracing along the strike with complete assurance that a definite hori
. Bulletin of the Geological Society of America. Geology. STRUCTURE 295 The means by which these several structural features are determined may be here pointed out. Such a statement will also serve to explain why only the major structural relations are determinable. CALCAREOUS Kp^ SLATE SERIES. LEGEND Cono/omer<9te Figure 1.—Sketch Map showing Pre-Cambrian Structure in northern Blaok Hills Within this series of schists there are only a few stratigraphic mem- bers which are sufficiently persistent and distinctive to permit tracing along the strike with complete assurance that a definite horizon is being. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Geological Society of America. [New York : The Society]
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Keywords: ., bookcentury1800, bookdecade1890, booksubjectgeology, bookyear1890
