Lihat sumber Templat:M/doc

*<small>For the "small letter m with dot below" please use the HTML encoding "&amp;7747;", or the Unicode "1E43" code.</small> 

Given a valid code (see table), outputs an earthquake magnitude scale label, either the generic {{M|.}}, or a subtype (such as {{M|w}} or {{M|blg}}), conformable with the labels most commonly used by the major seismological authorities. The article is automatically added to a tracking category. Optionally adds a value or relation, identifies a source, or links to explanatory text at [[Seismic magnitude scales]].

=== Penggunaan ===

* <code><nowiki>{{ M | <code*> | <value or relation> | src = <source> | link=y }}</nowiki></code>

Perlu '''kode''' yang benar (lihat [[#Tabel kode|tabel]]), parameter lain opsional.

===Contoh===

Label saja:
* {{tlx|M|w}}&nbsp;→ {{M|w}}

Dengan nilai atau jangkauan:
* {{tlx|M|s|5.1}}&nbsp;→ {{M|s|5.1}}.
* {{tlx|M|w|6.2 – 6.5}}&nbsp;→ {{M|w|6.2 – 6.5}}

Label yang ditautkan ke teks penjelas (berguna untuk entri pertama yang dicantumkan):
* {{tlx|M|t|'''link&#61;y'''}}&nbsp;→ {{M|t|link=y}}
* {{tlx|M|b|5.2|'''link&#61;y'''}}&nbsp;→ {{M|b|5.2|link=y}}

Untuk menunjukkan bahwa magnitudonya berasal dari katalog atau sumber lain, gunakan {{para|src}}:
* {{tlx|M|w|8.1|'''src&#61;'''HRV}}, {{tlx|M|e|8.8|'''src&#61;'''USGS-PDE}}&nbsp;→ {{M|w|8.1|src=HRV}}, &nbsp;&nbsp;{{M|e|8.8|src=USGS-PDE}}
:<small>(Catatan: ini tidak cocok untuk [[WP:Verifikasi]].)</small>

Ada banyak skala magnitudo. Untuk menjaga keakuratan dan menghindari kesalahan <b>''gunakan kode yang benar''</b> (lihat di bawah). 
Apabila Anda tidak yakin, gunakan kode khusus "?" supaya bisa diperbaiki oleh kontributor lain:
* {{tlx|M|?}}&nbsp;→ {{M|?}}

Contoh pemakaian di teks artikel dengan sitiran sebaris:
* {{tq|The 1964 Alaska earthquake, magnitude <nowiki>{{M|w|6.7|src=NEIC}}&lt;ref>{{short-isc|EHB|869809}}.&lt;/ref></nowiki> ....}}

Kode khusus "magnitude" menghasilkan tautan wiki untuk dipakai secara umum:
* {{tq|A {{m|magnitude}} 7 earthquake ....}}

Kode khusus "M" dan "mag" menghasilkan teks bertautan untuk dipakai di tabel:
* {{tlx|M|M}}&nbsp;→ {{M|M}}; {{tlx|M|mag}}&nbsp;→ {{M|mag}}

<div style="border: 2px solid #005000;margin: 2em; padding: 1em;">
{{hl|&nbsp;Important note: Please do NOT specify a magnitude as "Richter scale"}} just because a newspaper or other popular media says "Richter". '''That is usually incorrect'''. Earthquake magnitudes reported by the [[U.S. Geological Survey]] (USGS) and other seismological authorities now generally use the [[Seismic scale#Mw|moment magnitude scale]] for magnitudes greater than 4.0. While most newspapers and other popular media refer to this as the "Richter" magnitude, that is not correct. [[Richter magnitude scale|Richter's original scale]], explicitly denoted with the symbol "ML" or "M<sub>L</sub>" (where "L" indicates "Local"), was developed for measuring the magnitude of earthquakes in the vicinity of southern California.  While the "Richter" and moment magnitude scales are similar, they do differ, particularly for larger earthquakes.

In general: where any source specifies magnitude on a scale ''other than'' "Richter", or uses "M" (or "m") with one or more other letters (such as ML, Mw, Ms, or mb), that can be relied on; use the table below to match the label and determine the proper code.

Where a newspaper or other popular media refers to the scale or magnitude of a recent earthquake as "Richter" it is probably the popular mis-identification of the moment magnitude scale. Best practice is to check with an authoritative source, such as the USGS or the International Seismic Centre (see below).  USGS policy is that magnitudes in press releases, indicated as "M" without any additional characters, are implicitly moment magnitude. But: <b>do not use the "w" code</b> if the source <b>''does not actually say''</b> "M<sub>w</sub>" or "moment magnitude scale".  If you have a strong basis for believing moment magnitude is meant – e.g., because it is a USGS press release – use the "dot" code to indicate an ''implicit'' M<sub>w</sub>.  E.g.: {{tlx|M|<b>.</b>|5.7}}→ {{M|.|5.7}}; {{tlx|M|<b>.</b>|link&#61;}}→ {{M|.|link=y}}.

If you are not sure of the scale, use {{tlx|M|?}}.
</div>

=== Sumber data ===
{{hl|Newspapers and other mass media are ''not'' reliable sources for earthquake magnitudes.}} It is preferable that earthquake magnitudes always be obtained from '''authoritative sources''', such as the following.

* The '''ANSS''' (Advanced National Seismic System) '''Composite Catalog''', commonly known as "'''ComCat'''" is a near-realtime repository of earthquake information from the '''USGS''' (United States Geological Survey) and various regional data centers, with additional data from seismic networks around the world.  Event pages for significant events generally have an executive summary, a tectonic overview, past earthquake history of that area, [[ShakeMap]]s, and other material.  ComCat can be accessed in several ways:

:* [https://earthquake.usgs.gov/earthquakes/ Latest Earthquakes]. In most cases there is an initial report within 10 to 30 minutes of all magnitude 5.0+ earthquakes globally, and magnitude 4.0+ earthquakes within the contiguous U.S. Note that the magnitudes and locations in the initial reports are only first-order approximations, which get revised in the following hours, days, and months.

:* [https://earthquake.usgs.gov/earthquakes/browse/significant.php Significant Earthquakes archive]: a chronological listing of [https://earthquake.usgs.gov/earthquakes/browse/significant.php#sigdefsignificant events] since 1900.

:* [http://isc-mirror.iris.washington.edu/iscbulletin/search/catalogue/ Interactive search].

:All of these access methods link to event pages in the ANSS/ComCat catalog, which can be cited using {{tl|short-anss}} and {{tl|cite_anss}}.

* The '''ISC''' ([[International Seismological Centre]]) is the final and authoritative archive of global earthquake data. Services include:
:* The [http://www.isc.ac.uk/iscbulletin/search/catalogue/ On-Line Bulletin] ([http://isc-mirror.iris.washington.edu/iscbulletin/search/catalogue/ IRIS mirror]) incorporates several catalogs (databases). There are catalog-specific search functions for finding events constrained by date period, magnitude range, or region (by latitude and longitude, or [[Flinn-Engdahl regions]]). Data may be revised years later as more data is obtained or processes refined. This is the '''most complete, most authoritative, and preferred source''' for earthquake magnitudes and epicenters.
:* [http://www.isc.ac.uk/event_bibliography/eventindex.php Event Bibliography] ([http://isc-mirror.iris.washington.edu/event_bibliography/eventindex.php IRIS mirror]) of scientific articles for notable events, indexed chronologically. (Useful for finding ISC event id.) 
:* The [http://www.isc.ac.uk/iscgem/overview.php ISC-GEM Global Instrumental Earthquake Catalogue]: Definitive magnitudes for selected earthquakes since 1900. (Source id: GEM.)

:Data from the ISC can cited using {{tl|short-isc}} and {{tl|cite isc}}.

Earthquake magnitudes are given on different scales because they measure different aspects of the event. Estimates of magnitude may differ between networks and across time because of differences or changes in how the seismograms are read and the data processed. For details see the NMSOP-2 documentation (below).

=== Tabel kode ===
These are the most commonly found scales of earthquake ''magnitude''. Any scale not found in this table is mostly likely one of the following:
* An ''intensity'' scale. See [[Seismic intensity scales]] for explanation. This template does not cover intensity scales.
* A ''regional'' (or "local") scale used by some particular seismic network (or country). In general it is preferable to use one of the better known scales from the table. Exceptions are for historical reports; you will need to explicitly format as appropriate. If the scale has been properly calibrated (see MNSOP-2, Chapter 3, §3.2.4.3, p. 65) then "L" may be appropriate, along with the {{para|src}} parameter.
* A ''technical'' scale. While these might come up in an article related to seismology, they are not appropriate for general description of earthquakes. If needed, please format appropriately. On first use be sure to add a footnote explaining the scale. 

''Be careful to distinguish'' upper- and lower-case "M/m", "B/b", "L/<kbd>l</kbd>", and "<kbd>I/i</kbd>". Other than that case is generally not significant, nor italicization or subscripting. 

The following examples are representative, even comprehensive, but not complete.

{{refbegin}}
{|class=wikitable
|+ <big>Labels and codes for various earthquake magnitude scales</big>
|-
! colspan=5 | As seen in sources
! rowspan=2 | 
! rowspan=2 | WP
! rowspan=2 | Code
! rowspan=2 | Mag. scale
! rowspan=2 | Cat.
! rowspan=2 | #
! rowspan=2 | Comments
|-
!<small>IASPEI</small>
!<small>NMSOP</small>
!<small>USGS</small>
!<small>ISC</small>
!<small>BSSA</small>
|- #
| --|| --|| --|| --|| --||
|{{M|?}}  ||?  || Unspecified
|[[:Category:M_?|M_?]]||{{PAGESINCAT:M_?|R}}
|WP: scale is unspecified or indeterminate.
|- #
| --|| --|| --|| --|| --||
|{{M|??}} ||?? || Needs verification
|[[:Category:M_??|M_??]]||{{PAGESINCAT:M_??|R}}
|WP: the scale and/or magnitude needs verification.
|- #
| --|| --|| --|| --|| --||
|{{M|R?|link=y}}  ||R? || Dubious "Richter"
|[[:Category:M_R?|M_R?]]||{{PAGESINCAT:M_R?|R}}
|WP: "Richter" scale is asserted, but dubious.
|- ----------
|
|- #
| || || UK || || ||→
|{{M|uk|link=y}}  || uk  || Unknown
|[[:Category:M_uk|M_uk]]||{{PAGESINCAT:M_uk|R}}
|Source says "unknown" scale. Might be 1954 M<sub>GR</sub> mag. See [[Seismic magnitude scales#Muk|here]].
<!-- == Variations on Richter/Local == -->
|- #
| ML     || M<kbd>l</kbd> || ML  || M<sub>L</sub> || ''M''<sub>L</sub> ||→
|{{M|L|link=y}}  || <kbd>l</kbd> || [[Richter magnitude scale|Local ("Richter")]]
|[[:Category:M_L|M_L]]||{{PAGESINCAT:M_L|R}}
| §4.1 "Local" to Southern Calif. Adapted for other regions, but not necessarily comparable.
|- #
| || M<sub>JMA</sub> || Mj ||  || ''M''<sub>JMA</sub> ||→
|{{M|jma|link=y}} ||jma || JMA "Local" mag.
|[[:Category:M_jma|M_jma]]||{{PAGESINCAT:M_jma|R}}
| §3.2.4.7 Japanese Meteorological Agency. Also M<sub>J</sub>, but ''not'' M<sub>w</sub>(JMA).
|- ----------
|
<!-- == Variations on MOMENT magnitude == -->
|- #
| || || || || ''M''<sub>0</sub>||→
|{{M|0|link=y}}  ||0  || [[seismic moment]]
|[[:Category:M_0|M_0]]||{{PAGESINCAT:M_0|R}}
| "M zero". A physical value, basis of M<sub>w</sub>. In Newton-meters or dyne-centimeters
|- #
| || || M || ||<b>M</b>||→
|{{M|.|link=y}}  ||<b>.</b>  || [[Moment magnitude scale|moment mag.]]
|[[:Category:M_w.|M_w.]]||{{PAGESINCAT:M_w.|R}}
| dot: implicit Mw. 
|- #
| Mw || || Mw || || ''M''w||→
|{{M|w|link=y}}  ||w  || [[Moment magnitude scale|moment mag.]]
|[[:Category:M_w|M_w]]||{{PAGESINCAT:M_w|R}}
| §4.7 Generally preferred when available. Use ''only if'' "w" is present.
|- #
| || ||Mwb|| || ||→
|{{M|wb|link=y}}  ||wb  || 
|[[:Category:M_wb|M_wb]]||{{PAGESINCAT:M_wb|R}}
| M<sub>w</sub> calculated from body-waves
|- #
| || ||Mwc|| || ||→
|{{M|wc|link=y}}  ||wc  || 
|[[:Category:M_wc|M_wc]]||{{PAGESINCAT:M_wc|R}}
| M<sub>w</sub> from centroid moment
|- #
| || ||Mww|| || ||→
|{{M|ww|link=y}}  ||ww  || 
|[[:Category:M_ww|M_ww]]||{{PAGESINCAT:M_wc|R}}
| M<sub>w</sub> from W-phase centroid
|- #
| || ||Mwr|| || ||→
|{{M|wr|link=y}}  ||wr  || 
|[[:Category:M_wr|M_wr]]||{{PAGESINCAT:M_wr|R}}
| M<sub>w</sub> at regional distance
|- #
| || ||Mwp|| || ||→
|{{M|wp|link=y}}  ||wp  || 
|[[:Category:M_wp|M_wp]]||{{PAGESINCAT:M_wp|R}}
| M<sub>w</sub> from broadband P-waves §3.2.8.2
|- #
|Mwpd || ||  || || ||→
|{{M|wpd|link=y}}  ||wpd  || 
|[[:Category:M_wpd|M_wpd]]||{{PAGESINCAT:M_wpd|R}}
| M<sub>wp</sub> w/ duration §3.2.8.3
|- #
| || || M<sub><kbd>i</kbd></sub>  || || ||→
|{{M|i|link=y}}  || <kbd>i</kbd> || 
|[[:Category:M_i|M_i]]||{{PAGESINCAT:M_i|R}}
| Only if ''lower-case'' "<kbd>i</kbd>"! USGS synonym for Mwp?
|- ----------
| 
<!-- == Variations on BODY waves. == -->
|- #
| mb     || mb  || mb  || ''M''b || m<sub>b</sub> ||→
|{{M|b|link=y}}  ||b   || [[Body wave magnitude|body-wave, short-period]] 
|[[:Category:M_b|M_b]]||{{PAGESINCAT:M_b|R}}
| §4.3 ''Case sensitive'': use "b"
|- #
| mB  || mB  || --  || M  || ''M''<sub>b</sub>(BB) ||→
|{{M|B|link=y}} ||B  || [[Body wave magnitude|body-wave, broadband]] 
|[[:Category:M_B|M_B]]||{{PAGESINCAT:M_B|R}}
| §4.2 ''Case sensitive'': use "B"
|- #
| mB_BB  || mB  || --  || M  || ''M''<sub>b</sub>(BB) ||→
|{{M|bbb|link=y}} ||bbb || [[Body wave magnitude|body-wave, broadband]] 
|[[:Category:M_Bbb|M_Bbb]]||{{PAGESINCAT:M_Bbb|R}}
| §4.2 
|- #
| mb_Lg  || mbLg || mb_Lg, MLg ||  || ''m''<sub>b</sub>(L<sub>g</sub>) ||→
|{{M|blg|link=y}} ||b<kbd>l</kbd>g || mb from Lg wave 
|[[:Category:M_bLg|M_bLg]]||{{PAGESINCAT:M_bLg|R}}
| §3.2.4.4; §4.6 North America east of the [[Rocky Mountains]], and other [[cratons]]
|- #
|        ||      || Mn || MN ||  ||→
|{{M|N|link=y}} || n || Nuttli (1973)
|[[:Category:M_N|M_N]]||{{PAGESINCAT:M_N|R}}
| §3.2.4.4; §4.6  Same as mb<sub>Lg</sub>
|- #
| mBc    ||      ||    ||   ||  ||→
|{{M|bc|link=y}} || bc || Cumulative body-wave
|[[:Category:M_Bc|M_Bc]]||{{PAGESINCAT:M_Bc|R}}
| §3.2.8.1
|- --------
| 
<!-- == Variations on a SURFACE wave == -->
|- #
| || || || || ''M''<sub>S</sub>||→
|{{M|s|link=y}}  ||s  || [[Surface wave magnitude|surface wave]]
|[[:Category:M_s|M_s]]||{{PAGESINCAT:M_s|R}}
| §4.4  Generic
|- #
| Ms_20  || Ms  || Ms  || Ms   || ''M''<sub>s</sub>(20) ||→
|{{M|s20|link=y}} ||s20 || surface-wave 20s
|[[:Category:M_s20|M_s20]]||{{PAGESINCAT:M_s20|R}}
| §4.4 Short period (20 sec.) surface waves
|- #
| Ms_BB  || Ms  || --  || Ms   || ''M''<sub>s</sub>(BB) ||→
|{{M|sbb|link=y}} ||sbb || [[Surface wave magnitude|broadband surface wave]] 
|[[:Category:M_sbb|M_sbb]]||{{PAGESINCAT:M_sbb|R}}
| §4.5
|- #
| || || || || ||
|{{M|z|link=y}}  ||z  || surface wave, vertical 
|[[:Category:M_z|M_z]]||{{PAGESINCAT:M_z|R}}
| Used before measuring the vertical phase became standard.
|- #
| || || || || ''M''<sub>S7</sub>||→
|{{M|s7|link=y}}  ||s7  || surface wave 
|[[:Category:M_s7|M_s7]]||{{PAGESINCAT:M_s7|R}}
| On Chinese seismograph
|- #
| || || M<sub>Sn</sub> || || ||→
|{{M|sn|link=y}}  ||sn  || surface wave
|[[:Category:M_sn|M_sn]]||{{PAGESINCAT:M_sn|R}}
| 1-second period per Nuttli (1983)  
|- #
|  ||  || M<sub>GR</sub> || || ''M''<sub>GR</sub> ||→
|{{M|gr|link=y}}  || gr || [[Seismic scale#Mgr|Gutenberg-Richter]]
|[[:Category:M_gr|M_gr]]||{{PAGESINCAT:M_gr|R}}
| 1954 G-R version of M<sub>s</sub>. Includes M<sub>PAS</sub> ("Pasadena")
|- #
| || || M<sub>R</sub>  || || ||→
|{{M|r|link=y}}  || r || Rothe
|[[:Category:M_r|M_r]]||{{PAGESINCAT:M_r|R}}
|  ''Not'' "Richter"! M<sub>s</sub> per Rothe 1969
|- #
| || || MLH  || || ||→
|{{M|lh|link=y}}  || lh || Russian M<sub>s</sub>
|[[:Category:M_LH|M_LH]]||{{PAGESINCAT:M_LH|R}}
| Parts of Russia (Obninsk)
|- --------
|
<!-- misc. -->
|- #
| Mc || || || || ''M''<sub>c</sub>||→
|{{M|c|link=y}}  ||c  || coda length
|[[:Category:M_c|M_c]]||{{PAGESINCAT:M_c|R}}
| §3.2.4.5
|- #
| Md || || MD ||  || ''M''<sub>D</sub>||→
|{{M|d|link=y}}  ||d  || [[Earthquake duration magnitude|duration]]
|[[:Category:M_d|M_d]]||{{PAGESINCAT:M_d|R}}
| §3.2.4.5 Many variants. ''Not'' JMA displacement mag.
|- #
| || || || || ||
|{{M|t|link=y}}  ||t || tsunami mag.
|[[:Category:M_t|M_t]]||{{PAGESINCAT:M_t|R}}
| §3.2.6.7  Used by [http://ptwc.weather.gov/ PTWC]
|- #
| || || || || ''M''<sub>m</sub> ||→
|{{M|m|link=y}}  ||m  || mantle mag.
|[[:Category:M_m|M_m]]||{{PAGESINCAT:M_m|R}}
| §3.2.8.5  Used by [http://ptwc.weather.gov/ PTWC]
|- #
| || || || || ||
|{{M|e|link=y}}  ||e  || energy mag.
|[[:Category:M_e|M_e]]||{{PAGESINCAT:M_e|R}}
| §3.2.7.2
|- #
| || || K || || ||
| – || – || K-class
|[[:Category:K|K]]||{{PAGESINCAT:K|R}}
| See [[Energy class]]. Use [[:Template:K]]
|- #
| || || M(K) || || ||→
|{{M|k|link=y}}  ||k  || [[Seismic scale#MK|K-class mag.]]
|[[:Category:M_K|M_K]]||{{PAGESINCAT:M_K|R}}
| Mag. calculated from "energy class" K
|- --------
|
<!-- Macroseismic-based scales -->
|- #
| || || || || ||
|{{M|ms|link=y}}  || ms || macroseismic
|[[:Category:M_ms|M_ms]]||{{PAGESINCAT:M_ms|R}}
| §3.2.6.6 Generic mag. estimated from macroseismic effects
|- #
| || || FA || || ''M''<sub>fa</sub> ||→
|{{M|fa|link=y}}  || fa || m<sub>b</sub> from felt-area
|[[:Category:M_fa|M_fa]]||{{PAGESINCAT:M_fa|R}}
| Est. from extent of felt-area. Multiple methods. 
|- #
| || || M<sub>La</sub> || || ||→
|{{M|la|link=y}}  ||<kbd>l</kbd>a  || M<sub>L</sub> from felt-area
|[[:Category:M_la|M_la]]||{{PAGESINCAT:M_la|R}}
| M<sub>L</sub> est. from intensity reports; for Calif. and Hawaii
|- #
| || || M<sub><kbd>I</kbd></sub>  || || ||→
|{{M|I|link=y}}  || <kbd>I</kbd> || M<sub>L</sub> from intensity
|[[:Category:M_I|M_I]]||{{PAGESINCAT:M_I|R}}
| Only if ''upper-case'' "<kbd>I</kbd>"! Est. from epicentral intensity.
|- --------

|}

Examples of use are from the [http://www.iaspei.org International Association of Earth Physics and Interior] ('''IASPEI'''), the first edition of the [http://bib.telegrafenberg.de/publizieren/vertrieb/nmsop/nmsop-2002/ New Manual of Seismological Practice] ('''NMSOP''')(the second edition follows the IASPEI), the [[United States Geological Survey]] ('''USGS''') National Earthquake Information Center (NEIC), the [[International Seismological Centre]] ('''ISC'''), and the [[Bulletin of the Seismological Society of America]] ('''BSSA'''), as summarized in table 3 of the IASPEI/MNSOP-2 [http://gfzpublic.gfz-potsdam.de Information Sheet 3.3]. Additional magnitude scales from [http://gfzpublic.gfz-potsdam.de Chapter 3] of MNSOP-2, ISC documentation, the [https://earthquake.usgs.gov/earthquakes/eventpage/terms.php USGS], and a review of the literature. Section numbers under "Comments" are for either Chapter 3, or  Information Sheet 3.3

The nomenclature style implemented here is adapted from IASPEI/MNSOP-2 Information Sheet 3.3.  This style differs from IASPEI style mainly in using subscripts rather than underscores, and from BSSA style mainly in not using parentheses.
 
"Cat.": the Categories for tracking use of these various scales. "#" is the number of pages in that category (when last checked).

Principal references on usage are:
*{{Citation
 |editor1-first= P. |editor1-last= Bormann
 |date= 2012
 |title= New Manual of Seismological Observatory Practice 2 (NMSOP-2)
 |publisher= IASPEI/GFZ German Research Centre for Geosciences
 |place= Potsdam
 |doi= 10.2312/GFZ.NMSOP-2
 |url=  http://nmsop.gfz-potsdam.de
}}.

*{{Citation
 |ref= CITEREFIS 3.32014
 |first1= P. |last1= Bormann
 |first2= J. W. |last2= Dewey
 |date= 2014
 |chapter= Information Sheet 3.3: The new IASPEI standards for determining magnitudes from digital data and their relation to classical magnitudes.
 |chapter-url= http://gfzpublic.gfz-potsdam.de/pubman/item/escidoc:816929:1/component/escidoc:816928/IS_3.3_rev1.pdf
 |editor1-last= Bormann
 |title= New Manual of Seismological Observatory Practice 2 (NMSOP-2)
 |doi= 10.2312/GFZ.NMSOP-2_IS_3.3
 |url= http://bib.telegrafenberg.de/publizieren/vertrieb/nmsop/
}}.

These sources also have extensive discussion and references on the derivation and comparison of the various scales.

{{refend}}

==Lihat pula==
* {{cl|Articles using templated earthquake magnitude scale}}
* [[Seismic magnitude scales]]. Brief descriptions of the most common magnitude scales.
* [[Template:Cite anss]] For citing data from the USGS-[[ANSS]] Comprehensive Catalog.
* [[Template:Short-anss]] In-line short-cite.
* [[Template:Cite isc]] For citing data from the [[International Seismological Centre]].
* [[Template:Short-isc]] In-line short-cite.

<includeonly>
<!-- Categorization of the template itself -->
[[Category:Templat penanda satuan]]
[[Category:Templat karakter]]
[[Category:Pengukuran seismologi]]
[[Category:Templat gempa bumi|M]]
</includeonly>