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  2. Sequence stratigraphy - Wikipedia

    en.wikipedia.org/wiki/Sequence_stratigraphy

    Sequence stratigraphy is a branch of geology, specifically a branch of stratigraphy, that attempts to discern and understand historic geology through time by subdividing and linking sedimentary deposits into unconformity bounded units on a variety of scales.

  3. Type 1 and type 2 sequence - Wikipedia

    en.wikipedia.org/wiki/Type_1_and_type_2_sequence

    The definition of a type 1 and type 2 sequence was first introduced by Vail et al. (1984). [4] Since they were hard to recognize, they were redefined in 1990 by Van Wagoner et al.. However even with this new definition, type 2 sequence boundaries were hard to recognize in the field due to their lack of subaerial exposure.

  4. Sequence (geology) - Wikipedia

    en.wikipedia.org/wiki/Sequence_(geology)

    View history; Tools. Tools. move to sidebar hide. Actions Read; Edit; View history ... a sequence is a stratigraphic unit which is bounded by an unconformity at the ...

  5. Stratigraphy - Wikipedia

    en.wikipedia.org/wiki/Stratigraphy

    Stratigraphy is a branch of geology concerned with the study of rock layers and layering (stratification). It is primarily used in the study of sedimentary and layered volcanic rocks . Stratigraphy has three related subfields: lithostratigraphy (lithologic stratigraphy), biostratigraphy (biologic stratigraphy), and chronostratigraphy ...

  6. Cyclic sediments - Wikipedia

    en.wikipedia.org/wiki/Cyclic_sediments

    Sequence stratigraphy, the study of sea level change through the examination of sedimentary deposits, was developed from the centuries-old controversy over the origin of cyclic sedimentation and the relative importance of eustatic and tectonic factors on sea level change. [2]

  7. Historical geology - Wikipedia

    en.wikipedia.org/wiki/Historical_geology

    During the 17th century, Nicolas Steno was the first to observe and propose a number of basic principles of historical geology, including three key stratigraphic principles: the law of superposition, the principle of original horizontality, and the principle of lateral continuity.

  8. Cratonic sequence - Wikipedia

    en.wikipedia.org/wiki/Cratonic_sequence

    A cratonic sequence (also known as megasequence, Sloss sequence or supersequence) in geology is a very large-scale lithostratigraphic sequence in the rock record that represents a complete cycle of marine transgression and regression on a craton (block of continental crust) over geologic time.

  9. Parasequence - Wikipedia

    en.wikipedia.org/wiki/Parasequence

    View history; Tools. Tools. move to sidebar ... A parasequence is a fundamental concept of sequence stratigraphy. ... which is sometimes also included into the ...