WebA search for the source of this anomaly was unsuccessful other than that a float sample collected nearby contained traces of galena, pyrrhotite, and chalcopyrite. The site is at or near the contact between Cretaceous biotite schist and Tertiary or Cretaceous tonalite (Brew and Grybeck, 1984). Geologic map unit (-133.12193858895, 57.5997343299991) WebJan 1, 2024 · The Early Cretaceous tonalite forms a ~150–350 m-wide zone adjacent to the Paposo fault (Fig. 2, Supplementary File 1). This unit is mostly protomylonitic with very low strain zones near the contact with the hydrothermally-altered granodiorite complex along the tonalite's eastern margin. The tonalite grades from protomylonite to intensely ...
Green Valley Tonalite (Cretaceous) - MiraCosta College
WebTonalite and trondhjemite (Cretaceous)—Biotite- and hornblende-biotite tonalite and biotite-muscovite trondhjemite (120-110 Ma); rocks contain conspicuous magmatic epidote in plutons along eastern edge of arc complex. Includes tonalitic part of Hazard Creek complex northwest of McCall, Blacktail pluton southeast of Grangeville, and Sixmile ... rbackup support
Comparison of Late Cretaceous Plutonic rocks across …
WebThe concealed location of the San Jacinto Fault Zone shown on this quadrangle is after Sharp, 1967. The geology of the quadrangle is dominated by Cretaceous tonalite formerly included in the Coahuila Valley pluton of Sharp (1967). The northern part of Sharp's Coahuila Valley pluton is separated out as the Hemet pluton. Tonalite of the Hemet... WebNov 1, 2024 · A detailed petrographic, geochemical and geochronological study reveals a suite of Miocene (~21–23 Ma) high Sr/Y and La/Yb volcanic rocks of dacite compositions and adjacent Late Cretaceous tonalite and granodiorite (~78–80 Ma) in the Qiewa of the southern Gangdese batholith. WebGeologic Description = Jasper (1967) reports scattered occurrences of copper mineralization, most likely copper stain, in Tertiary to Late Cretaceous tonalite. There is no visible continuity between occurrences. Age = Late Cretaceous or younger; host is Tertiary to Late Cretaceous tonalite. Age = Host rock is Tertiay - Late Cretaceous. duc ma lavang san jose