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Source: The Open Library

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1Sedimentation and stratigraphy of carbonate rock sequences

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“Sedimentation and stratigraphy of carbonate rock sequences” Metadata:

  • Title: ➤  Sedimentation and stratigraphy of carbonate rock sequences
  • Author:
  • Language: English
  • Publisher: American Geophysical Union
  • Publish Date:
  • Publish Location: Washington, D.C

“Sedimentation and stratigraphy of carbonate rock sequences” Subjects and Themes:

Edition Identifiers:

Access and General Info:

  • First Year Published: 1989
  • Is Full Text Available: Yes
  • Is The Book Public: No
  • Access Status: Borrowable

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Shallow water marine environment

forms readily in shallow, warm, calm waters. While siliciclastic and carbonaceous sediments can coexist, shallow marine environments can also contain only

Organic-rich sedimentary rocks

bitumen, asphalt, petroleum, coal or carbonaceous material. Organic-rich sedimentary rocks may act as source rocks which generate hydrocarbons that accumulate

Inertinite

(2023-02-22). Carbon permanence of biochar; a lesson learned from the geologically preserved charcoal in carbonaceous rocks (Report). Copernicus Meetings. v t e

Skarn

composition of protolith or surrounding rocks. Uncommon types of skarns are formed in contact with sulfidic or carbonaceous rocks such as black shales, graphite

Loire

siliceous fragmented rocks with groundwater occurring in fissures. The sedimentary domain consists of limestone and carbonaceous rocks, that, where saturated

Chicxulub crater

characteristics of CM or CR carbonaceous chondrites. Ruthenium isotope ratios found in impact layers also support a carbonaceous chondrite composition for

Chondrite

ratios of 17O/16O relative to 18O/16O, when compared to Earth rocks. All groups of carbonaceous chondrites except the CH group are named for a characteristic

Biochar carbon removal

biochar; a lesson learned from the geologically preserved charcoal in carbonaceous rocks (Report). Copernicus Meetings. Chiaramonti, David; Lotti, Giulia;

C-type asteroid

C-type (carbonaceous /ˌkɑːrbəˈneɪʃəs/) asteroids are the most common variety, forming around 75% of known asteroids. They are volatile-rich and distinguished

Precambrian

include a possible 2450 Ma red alga from the Kola Peninsula, 1650 Ma carbonaceous biosignatures in north China, the 1600 Ma Rafatazmia, and a possible