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STRUCTURAL GEOLOGY

STRUCTURAL GEOLOGY
11問 • 1年前
  • Aira Moral
    • 通報

    問題一覧

  • 1

    The branch of geology that deals with the form, arrangement, and internal structure of the rocks, and esp. with the description, representation, and analysis of structures, chiefly on a moderate to small scale. The subject is similar to tectonics, but the latter is generally used for the broader regional or historical phases

    structural geology

  • 2

    defined as a geometric feature in a rock whose form, shape and distribution can be described. These features are separated into primary, secondary, tectonic and non-tectonic structures.

    geological structure

  • 3

    structures that are acquired during the genesis of a rock

    primary structure

  • 4

    locally driven or small scale features not immediately due to tectonic interaction.

    non-tectonic structures

  • 5

    theorizes that the Earth has largely been shaped by sudden,short-lived, violent events, possibly worldwide in scope.

    catastrophism

  • 6

    popularized the concept of catastrophism in the early 19th century; he proposed that new life-forms had moved in from other areas after local floods, and avoided religious or metaphysical speculation in his scientific writings

    Georges Cuvier

  • 7

    sometimes called gradualism

    uniformitarianism

  • 8

    according to which slow incremental changes, such as erosion, brought about all the Earth's geological features. explanations for the formation of sedimentary rock and an understanding of the immense stretch of geological time, or as the concept came to be known deep time, were found in the writing of James Hutton, sometimes known as the father of geology, in the late 18th century.

    uniformitarianism

  • 9

    built upon Hutton's ideas during the first half of 19th century and amassed observations in support of the uniformitarian idea that the Earth's features had been shaped by same geological processes that could be observed in the present acting gradually over an immense period of time.

    Charles Lyell

  • 10

    MAIN PRINCIPLES AND CONCEPTS OF SEDIMENTARY PETROLOGY

    Original Horizontality (Steno) Law of Superposition Principle of Cross-cutting Relationships Principle of Lateral Continuity

  • 11

    states that layers of sediment are originally deposited horizontally under the action of gravity.

    original horizontality

    • metallurgy

    metallurgy

    Aira Moral · 100問 · 1年前

    metallurgy

    metallurgy

    100問 • 1年前
    Aira Moral

    metallurgy 2

    metallurgy 2

    Aira Moral · 52問 · 1年前

    metallurgy 2

    metallurgy 2

    52問 • 1年前
    Aira Moral

    EXAM NO: 1 : GEOLOGY AND MINING TERMS

    EXAM NO: 1 : GEOLOGY AND MINING TERMS

    Aira Moral · 100問 · 1年前

    EXAM NO: 1 : GEOLOGY AND MINING TERMS

    EXAM NO: 1 : GEOLOGY AND MINING TERMS

    100問 • 1年前
    Aira Moral

    EXAM 2: Geology and Mining Terms

    EXAM 2: Geology and Mining Terms

    Aira Moral · 50問 · 1年前

    EXAM 2: Geology and Mining Terms

    EXAM 2: Geology and Mining Terms

    50問 • 1年前
    Aira Moral

    EXAM 3

    EXAM 3

    Aira Moral · 80問 · 1年前

    EXAM 3

    EXAM 3

    80問 • 1年前
    Aira Moral

    Principles of Mining

    Principles of Mining

    Aira Moral · 25問 · 1年前

    Principles of Mining

    Principles of Mining

    25問 • 1年前
    Aira Moral

    MINERALS

    MINERALS

    Aira Moral · 51問 · 1年前

    MINERALS

    MINERALS

    51問 • 1年前
    Aira Moral

    master

    master

    Aira Moral · 5問 · 1年前

    master

    master

    5問 • 1年前
    Aira Moral

    問題一覧

  • 1

    The branch of geology that deals with the form, arrangement, and internal structure of the rocks, and esp. with the description, representation, and analysis of structures, chiefly on a moderate to small scale. The subject is similar to tectonics, but the latter is generally used for the broader regional or historical phases

    structural geology

  • 2

    defined as a geometric feature in a rock whose form, shape and distribution can be described. These features are separated into primary, secondary, tectonic and non-tectonic structures.

    geological structure

  • 3

    structures that are acquired during the genesis of a rock

    primary structure

  • 4

    locally driven or small scale features not immediately due to tectonic interaction.

    non-tectonic structures

  • 5

    theorizes that the Earth has largely been shaped by sudden,short-lived, violent events, possibly worldwide in scope.

    catastrophism

  • 6

    popularized the concept of catastrophism in the early 19th century; he proposed that new life-forms had moved in from other areas after local floods, and avoided religious or metaphysical speculation in his scientific writings

    Georges Cuvier

  • 7

    sometimes called gradualism

    uniformitarianism

  • 8

    according to which slow incremental changes, such as erosion, brought about all the Earth's geological features. explanations for the formation of sedimentary rock and an understanding of the immense stretch of geological time, or as the concept came to be known deep time, were found in the writing of James Hutton, sometimes known as the father of geology, in the late 18th century.

    uniformitarianism

  • 9

    built upon Hutton's ideas during the first half of 19th century and amassed observations in support of the uniformitarian idea that the Earth's features had been shaped by same geological processes that could be observed in the present acting gradually over an immense period of time.

    Charles Lyell

  • 10

    MAIN PRINCIPLES AND CONCEPTS OF SEDIMENTARY PETROLOGY

    Original Horizontality (Steno) Law of Superposition Principle of Cross-cutting Relationships Principle of Lateral Continuity

  • 11

    states that layers of sediment are originally deposited horizontally under the action of gravity.

    original horizontality