Pg. 343-352. Isabella granodiorite. A large, generally massive, rather variable intrusive body consisting mainly of granodiorite. Grades into granite, also through quartz diorite into diorite. Is distinctly younger than the gabbro diorite that cuts Kernville series. May be Late Jurassic. It more or less intricately cuts Kernville series and the intrusive gabbro diorite.
Typical occurrence in vicinity of Isabella, Kernville quadrangle, Kern Co., southern CA.
Source: US geologic names lexicon (USGS Bull. 896, p. 1027).
Pg. 357-358, 378 (fig. 31), pl. 2. Isabella granodiorite. Shown on map and columnar section as Jurassic(?).
Source: US geologic names lexicon (USGS Bull. 1200, p. 1889).
Pg. 512, table 4. Isabella granodiorite. Late Mesozoic.
Source: US geologic names lexicon (USGS Bull. 1200, p. 1889).
Pg. F181-F189, pls. Isabella granodiorite. Lead (Pb)-alpha age determinations range from 85 to 96 million years. Average age is 90 million years, nearly equivalent to beginning of Late Cretaceous epoch. Younger than Kernville series.
Source: US geologic names lexicon (USGS Bull. 1200, p. 1889).
Pg. 9, geologic time scale (inside front cover). Isabella Granodiorite of Miller (1931). Sample from Lat. 35 deg. 34 min. 00 sec. N., Long. 118 deg. 34 min. 00 sec. W., Miracle Hot Springs quadrangle, Kern County, California, yielded a Pb-alpha age of 100 +/-10 Ma (zircon) [Cretaceous]. Age published by Marvin, 1968 (USGS Misc. Geol. Inv. Map I-537). Age calculated using decay constants of Steiger and Jager, 1977 (Earth Planet. Sci. Letters, v. 36, p. 359-362). Jaffe and others, 1959 (USGS Bull. 1097-B) reported Pb-alpha ages of 83, 89, and 96 Ma for similar zircon concentrates from same locality.
Source: Publication.
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