Lithostratigraphic Nomenclature Flashcards

1
Q

When was the Int’l Subcommission on Stratigraphic Terminology Report on the Principles of Stratigraphic Classification and Terminlogy made?

A

1961

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2
Q

When was the GSP Philippine Code of Stratigraphic Nomenclature made?

A

1968

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3
Q

When was the International Stratigraphic Guide made?

A

1976

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4
Q

When was the 2nd edition of Int’l Stratigraphic Guide made?

A

1994

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5
Q

When was the GSP Committee on Stratigraphic Nomenclature made?

A

1997

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6
Q

When was the Publication of Philippine Stratigraphic Guide made?

A

2001

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7
Q

Basic units of geologic mapping and essential element of the stratigraphy of an area. It is not defined by inferred age, time span they represent and manner of formation.

A

Lithostratigraphic units

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8
Q

Should possess a certain degree of internal lithologic homogeneity or distinctive lithologic features. It may consist of 1)one lithologic typel 2) repetitions of two or more lithologic types. Lithologic heterogeneity, in itself, may constitute a form of unity when compared to the adjacent rock units. In addition it should be mappable at a scale of 1:25,000.

A

Formation

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9
Q

Include chemical and mineralogical composition, texture, and such supplementary features as color, primary sedimentary structures or volcanic depositional structures, fossils (viewed as rock-forming particles), or other organic content (coal, oil-shale)

A

Lithologic characteristics of Formation

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10
Q

Not a determining parameter; may range from less than a meter to thousands of meters as long as it is mappable.

A

Thickness of Formation

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11
Q

Organic reefs and carbonate mounds may be distinguished formally as formations and distinct from their surrounding thinner, temporal equivalents.

A

Organic reefs and carbonate mounds of formation

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12
Q

Sedimentary and volcanic rocks that are interbedded may be assembled into a formation under one name, which should indicate the predominant or distinguishing lithology

A

Interbedded volcanic and sedimentary rocks formation

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13
Q

Mappable, distinguishable sequences of stratified volcanic rocks should be treated as lithostratigraphic units, as formations or as units of higher or lower rank. A small intrusive component of a dominantly stratiform volcanic assemblage may be treated informally, e.g. dikes, sills.

A

Volcanic rocks of formation

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14
Q

Distinguished mainly by lithologic characteristics.

A

Metamorphic rocks of formation

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15
Q

It is a named entity within a formation having characteristics that distinguish it from other parts of a formation. It may not be mappable at the scale required for formations.

A

Member

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16
Q

A geographically restricted unit that terminates on all sides laterally within a formation may be called a ______. A wedging unit may be called a _________.

A

Lens and tongue

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17
Q

Although members are normally in vertical sequence, laterally equivalent parts of a formation that differ recognizably may also be considered members.

A

Laterally equivalent members

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18
Q

May be divided into beds or (volcanic) flows

A

Division of members

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19
Q

The smallest formal lithostratigraphic unit of sedimentary rocks should be limited to certain distinctive _________ whose recognition is particularly useful. Coal, oil sands, and other of economic importance commonly are named.

A

Bed

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20
Q

the smallest formal lithostratigraphic unit of volcanic rocks. The designation should be limited to those that are distinctive and widespread.

A

Flow

21
Q

Defined to express the natural relationships of associated formations. They are useful in regional mapping and stratigraphic analysis

A

Group

22
Q

Example of a Flow

A

Taal Caldera, designating the flow units as Alitagtag Pumice Flow, Caloocan Pumice Flow, Sambong Ignimbrite and Taal Scoria Flow.

23
Q

Example of a Group

A

Caraballo Group in northeastern Sierra Madre of Luzon, consisting of volcano-sedimentary formations designated as Formations I, II and III

24
Q

T or F. Raising the rank of the unit is preferable to restricting the old name to a part of its former content, because a change in rank leaves the sense of a well-established unit unchanged.

A

T

25
Q

T or F. The initial letters of all words used in forming the names of formal rock-stratigraphic units are capitalized.

A

T

26
Q

Compound terms (e.g. carbonaceous shale) and terms that are not in common usage (calcirudite,) should be avoided. Combined terms, such as “sand and clay” should not be used for the lithologic part of the names .

A

Please read

27
Q

Should indicate the predominant or diagnostic lithology, even if subordinate lithologies are included. The simplest generally acceptable term is recommended (e.g. limestone, sandstone);

A

Please read

28
Q

T or F. Members designated solely by lithologic character (e.g. limestone member), by position (upper, lower) or by letter or number are informal.

A

T

29
Q

When geographic names are applied to such as oil sands, coal beds, mineralized zones, and informal members, the unit term should not be capitalized.

A

Informal units

30
Q

The name of beds or flows may combine a geographic term, lithologic term (optional) and the term “Bed” or “Flow”

A

Please read

31
Q

Geographic names should be derived from permanent natural or artificial features at or near the place where the stratigraphic unit is present. Names derived from such impermanent sources as farms, churches, schools, crossroads, and small communities are not entirely satisfactory but are acceptable if no others are available.

A

Please read

32
Q

The original or subsequently designated type section of a named layered stratigraphic unit or of a stratigraphic boundary representing a specific interval or point in a specific sequence of rock strata, and constituting the standard for the definition and characterization of the stratigraphic unit or boundary.

A

Stratotype

33
Q

The original stratotype designated by the original author

A

Holostratotype

34
Q

A supplementary stratotype used in the original definition to illustrate the heterogeneity of the stratigraphic unit

A

Parastratotype

35
Q

A stratotype for a previously described stratigraphic unit selected later in the absence of an adequately designated original stratotype.

A

Lectostratotype

36
Q

A new stratotype selected to replace the older one which has been destroyed, covered, or otherwise made inaccessible

A

Neostratotype

37
Q

A stratotype proposed after the original designation of the holostratotype (and parastratotype) in order to extend knowledge of the unit or boundary to other geographic areas.

A

Hypostratotype

38
Q

A description of the locality and map should enable anyone to find the stratotype. Photos would also help.

A

Geographic

39
Q

Lithology, thickness, structure, distribution, texture and composition, paleontology, geomorphic expression, and other geologic features of the type section.

A

Geologic

40
Q

T or F. Adjectives used as nouns, such as “volcanics,” “metamorphics,” “intrusives,” and “extrusives,” preferably should not be used in naming igneous and metamorphic rock bodies. However, they may be reluctantly accepted in formal lithostratigraphic nomenclature when judged useful.

A

T

41
Q

May be used to describe a diverse assemblage produced by volcanic activity to include extrusive volcanic rocks, related intrusions and associated pyroclastic deposits.

A

Volcanic complex

42
Q

The term “_______” has been commonly used for associations of apparently co-magmatic intrusive igneous rock bodies of similar or related rock lithologies and close association in time, space, and origin.

A

suite

43
Q

Assemblages of rock bodies with distinct lithologic characteristics and genetic associations. In a sense, they are a special class of complexes. A complete sequence consists of the following, from the bottom to the top: amphibolite, residual peridotite (harzburgite), transition zone dunite, layered ultramafic cumulates, layered gabbro, isotopic high level gabbro, sheeted dikes/sills complex, pillow basalt and pelagic sedimentary rocks.

A

Ophiolite sequences

44
Q

In case the assemblage does not represent a complete ophiolite sequence, the composite body may be called an __________.

A

ophiolitic complex

45
Q

Defined as a body of mappable rock unit (1:50,000) characterized both by the lack of internal continuity of contacts or strata and by the inclusion of fragments and blocks of all sizes, both exotic and native, in a matrix of finer-grained material.

A

Melange

46
Q

Also known as “sedimentary melange”, consists of a chaotic mass of rock with large clasts older than the enclosing sedimentary sequence.

A

Olistostromes

47
Q

Gigantic versions of olistostromes are called ________.

A

olistoliths

48
Q

Example of olistoliths in the Philippines

A

Codon Formation in Catanduanes with olistoliths of Bonagbonag Limestone.