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National Geologic Map Database
Geologic Unit: Julian
Map showing publication footprint
  • Usage in publication:
    • Julian group
  • Modifications:
    • Named
  • Dominant lithology:
    • Schist
  • AAPG geologic province:
    • Peninsular Ranges province
Publication:

Merrill, F.J.H., 1914, Geology and mineral resources of San Diego and Imperial Counties [California]: California State Mining Bureau, 113 p.


Summary:

Named for exposures near town of Julian, San Diego Co. and Imperial Co., CA. [no type section designated] Consists of mica schists, slates, quartzites, and limestone. Regarded as possibly lithologically and structurally equivalent to the Calaveras Group. Assigned Carboniferous(?) or older age

Source: GNU records (USGS DDS-6; Menlo GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Julian schist
  • Modifications:
    • Age modified
    • Revised
  • AAPG geologic province:
    • Peninsular Ranges province
Publication:

Hudson, F.S., 1922, Geology of the Cuyamaca region of California with special reference to the origin of nickeliferous pyrrhotite: University of California Publications in Geological Sciences, v. 13, no. 6, p. 175-252.


Summary:

Formerly designated "Julian group" (Merrill, 1914), now called Julian schist or Julian schist series. Mapped in Cuyamaca region. Consists of quartz-mica schists, amphibolite schists, paragneiss, and quartzite. Is more than 6,600 feet. thick. Intruded by Stonewall quartz diorite. Is Triassic(?) age indicated by ammonite float specimen (Smith, oral communication).

Source: GNU records (USGS DDS-6; Menlo GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Julian schist
  • Modifications:
    • Age modified
  • AAPG geologic province:
    • Peninsular Ranges province
Publication:

Donnelly, Maurice, 1934, Geology and mineral deposits of the Julian district, San Diego County, California: California Journal of Mines and Geology, v. 30, no. 4, p. 331-370.


Summary:

Assigned to Jurassic-Triassic(?) age based on lithologic and structural correlation with Calaveras formation (mainly Carboniferous) and with Santa Ana slates (Late Triassic) of the Santa Ana Mountains.

Source: GNU records (USGS DDS-6; Menlo GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Julian schist
  • Modifications:
    • Areal extent
  • AAPG geologic province:
    • Peninsular Ranges province
Publication:

Miller, W.J., 1935, A geologic section across the southern Peninsular Range of California: California Journal of Mines and Geology, v. 31, no. 2, p. 115-142, (incl. geologic map)


Summary:

Pg. 120-121. Julian schist of southern Peninsular Range [San Diego County, southern California] is same as Julian group of Merrill and Julian schist of Hudson. No fossils found. May include rocks of Triassic, late Paleozoic, or even older ages. Evidence obtained strongly suggests it is largely or wholly metamorphosed Triassic sediments.
Extended geographically and mapped in area across Peninsular Range near highway for 70 mi. from La Mesa to Coyote Wells.

Source: US geologic names lexicon (USGS Bull. 896, p. 1058); supplemental information from GNU records (USGS DDS-6; Menlo GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Julian schist
  • Modifications:
    • Mapped
  • AAPG geologic province:
    • Peninsular Ranges province
Publication:

Creasey, S.C., 1946, Geology and nickel mineralization of the Julian-Cuyamaca area, San Diego County, California: California Journal of Mines and Geology, no. 42, p. 15-29.


Summary:

Mapped in Julian-Cuyamaca area, San Diego Co., CA at scale 1" to 2000 feet.

Source: GNU records (USGS DDS-6; Menlo GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Julian schist
  • Modifications:
    • Areal extent
  • AAPG geologic province:
    • Peninsular Ranges province
Publication:

Merriam, Richard, 1946, Igneous and metamorphic rocks of the southwestern part of the Ramona quadrangle, San Diego County, California: Geological Society of America Bulletin, v. 57, no. 3, p. 223-260.


Summary:

Extended into and mapped in southwest part of Ramona 30' quad., San Diego Co., CA. Assigned Triassic(?) age. [no basis given]

Source: GNU records (USGS DDS-6; Menlo GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Julian schist*
  • Modifications:
    • Mapped
  • AAPG geologic province:
    • Peninsular Ranges province
Publication:

Everhart, D.L., 1951, Geology of the Cuyamaca Peak quadrangle, San Diego County, California: California Division of Mines Bulletin, no. 159, p. 51-115, (incl. geologic map, scale 1:62,500)


Summary:

Mapped in Cuyamaca Peak 15' quad., San Diego Co., CA. Map also includes Julian Schist and Stonewall Granodiorite undivided.

Source: GNU records (USGS DDS-6; Menlo GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Julian schist*
  • Modifications:
    • Mapped
  • AAPG geologic province:
    • Peninsular Ranges province
Publication:

Map showing publication footprint
  • Usage in publication:
    • Julian schist*
  • Modifications:
    • Areal extent
  • AAPG geologic province:
    • Peninsular Ranges province
Publication:

Gastil, R.G., 1961, The Mesozoic framework, IN Guidebook for field trips; San Diego County-1961: Geological Society of America, Cordilleran Section, Guidebook for Field Trips, 57th annual meeting, San Diego, CA, p. 4-7.


Summary:

Certain rocks in western San Diego Co., previously ascribed to "Julian Schist" are actually Alisitos Formation.

Source: GNU records (USGS DDS-6; Menlo GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Julian schist*
  • Modifications:
    • Mapped
  • AAPG geologic province:
    • Peninsular Ranges province
Publication:

Weber, F.H., Jr., 1963, Geology and mineral resources of San Diego County, California: California Division of Mines and Geology County Report, no. 3, 309 p.


Summary:

Julian Schist and Bedford Canyon Formation are mapped "undivided" but map states Julian Schist is in northeast, central and southeast parts of San Diego Co.

Source: GNU records (USGS DDS-6; Menlo GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Julian Schist*
  • Modifications:
    • Age modified
  • AAPG geologic province:
    • Peninsular Ranges province

Map showing publication footprint
  • Usage in publication:
    • Julian Schist*
  • Modifications:
    • Areal extent
  • AAPG geologic province:
    • Peninsular Ranges province
Publication:

Gastil, R.G., Phillips, R.P., and Allison, E.C., 1975, Reconnaissance geology of the State of Baja California: Geological Society of America Memoir, 140, 184 p.


Summary:

Quartzite-phyllite sequence at the south end of Sierra San Pedro Martir, State of Baja California, Mexico resembles the Julian Schist of San Diego Co., CA. Discontinuously exposed rocks extend southeastward. Suggests Triassic(?) and Jurassic(?) age based on analogy to areas north of border.

Source: GNU records (USGS DDS-6; Menlo GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Julian Schist*
  • Modifications:
    • Areal extent
  • AAPG geologic province:
    • Peninsular Ranges province
Publication:

Map showing publication footprint
  • Usage in publication:
    • Julian Schist*
  • Modifications:
    • Mapped
  • AAPG geologic province:
    • Peninsular Ranges province
Publication:

Lillis, P.G., Walawender, M.J., Smith, T.E., and Wilson, J., 1979, Petrology and emplacement of the Corte Madera gabbro pluton, southern California; [Field trip no. 5], IN Abbott, P.L., and Todd, V.R., eds., Mesozoic crystalline rocks; Peninsular Ranges batholith and pegmatites, Point Sal Ophiolite; Field trip nos. 5, 20-21, 24: Geological Society of America Field Trip Guidebook, [92nd] annual meeting, San Diego, CA, November 8-9, 1979, p. 143-150.


Summary:

Consists primarily of quartz-cordierite-biotite schist and quartz-diopside gneiss. Exposed throughout batholith. Sketch mapped in Corte Madera pluton. Although distribution overlaps that of Santiago Peak Volcanics no evidence is observed for structural relationship. Is no younger than Triassic(?) based on stratigraphic relations.

Source: GNU records (USGS DDS-6; Menlo GNULEX).


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Asterisk (*) indicates published by U.S. Geological Survey authors.

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