分享有关常用地球物理数据的笔记，希望对大家有益。9 N) U2 g. n. w# d8 R4 z
( d& ^8 W9 f U, ?1、GSRM-APM-1 Absolute Plate Motion Velocities:0 `7 R0 L/ A4 S0 Q% Z* P
0 J- R7 u9 H1 N/ k
Website Link: http://earthref.org/ERDA/972/
0 w/ H$ s! N$ G2 \) E! c
- j9 N' M. z! ]( Z0 Z6 c- Z! XSource description: Kreemer 2009, Absolute Plate Motions Constrained by Shear WaveSplitting Orientations with Implications for Hotspot Motions and Mantle Flow,J. Geophys. Res., VOL. 114, B10405, doi:10.1029/2009JB006416.0 S. s* h8 Q0 I2 \
. j+ z7 d5 M N: H: S8 a- i2、Crustal Age
9 J [, Q9 _" r' j1 x+ ^( H, u. l" O; @5 D, W6 y
Website Link: www.52ocean.cn& H! d( y' z9 Z: t# a% p, k2 V. B
& \+ H7 w* i* z: X& U9 X7 g: M+ Y
Source description: Müller, R.D., M. Sdrolias, C. Gaina, and W.R. Roest 2008. Age,spreading rates and spreading symmetry of the world's ocean crust, Geochem.Geophys. Geosyst., 9, Q04006,doi:10.1029/2007GC001743# j" {3 E$ e/ ^
! b" h! i$ t5 H2 ^4 G3、Spreading Rate
, i% U7 Y! L, s; L6 Q' A' O9 U0 X$ G. H) X2 T1 S
Website Link: www.52ocean.cn7 Z: j$ |- `- i F' H
. C6 j2 A f Y4 g" _7 B/ V7 ~/ @Source description: Müller, R.D., M. Sdrolias, C. Gaina, and W.R. Roest 2008. Age,spreading rates and spreading symmetry of the world's ocean crust, Geochem.Geophys. Geosyst., 9, Q04006,doi:10.1029/2007GC001743." x) b G U. |: j/ b8 l4 C8 \
3 B9 m% ^" O, b: m0 o9 W0 g! [4、Sediment Thickness+ C2 {" r: [4 M7 R0 b" o1 t/ h
7 N- O+ V j ]; L& n; ]. |8 t1 EWebsite Link: www.52ocean.cn5 |/ C& v9 f9 ~$ ~! M
( P" z0 \. g# u' j2 L
Source description: Divins, D.L., Total Sediment Thickness of the World's Oceans &Marginal Seas, NOAA National Geophysical Data Center, Boulder, CO, 2003.
8 H* v+ ~* @8 R- L" |) Q( i& C5 Y' W$ L$ A
5、Bathymetry & Topography% J a6 d2 y' }$ M
! X: Q/ @) V9 N( p' a2 O5 D
Website Link1: www.52ocean.cn3 L. V8 z$ r/ R' S* c
8 P$ F' T/ I* Q) p( f2 i, `0 T& cSource 1 description: ETOPO1 is a 1 arc-minute global relief model of Earth's surface thatintegrates land topography and ocean bathymetry.& ?7 a" V! }2 f8 }- e& O
2 ?& R6 E* s0 K& @
Website Link2: www.52ocean.cn
4 X" T* d& i- z0 M1 y/ K1 i
" I, J" k8 X: F* _- {Source 2 description: The General Bathymetric Chart of the Oceans (GEBCO) consists of aninternational group of experts who work on the development of a range ofbathymetric data sets and data products, including gridded bathymetric datasets, the GEBCO Digital Atlas, the GEBCO world map and the GEBCO Gazetteer ofUndersea Feature Names. [6 x; W6 J4 w# ~; p
! B4 w( X7 v* b' @9 ^: B6、Multibeam Bathymetry: @7 g1 ?4 Y5 A; @" _5 X9 `3 Q
; ~- A, W# ^- t( l1 }8 @Website Link1: www.52ocean.cn
" E9 l) w! x2 }8 t, \. J; E
" Z O2 M, U. X, O7 vSource 1 description: NGDC is the US national archive for multibeam bathymetric data andpresently holds over 15.7 million nautical miles of ship tracklines (1187surveys) received from sources worldwide.In addition to deepwater data, the multibeam database also includeshydrographic multibeam survey data from NOAA's National Ocean Service (NOS).
; V2 K* l6 `0 d6 }. l. R& \& Z8 K& x
9 R3 h% |4 Q8 W3 f' |- q- y5 FWebsite Link2: www.52ocean.cn
* g( [4 X/ s# M/ V8 W9 G ^* X% \3 ~6 Q9 f% r- [
Source 2 description: The Global Multi-Resolution Topography (GMRT)synthesis is a compilation of multibeam sonar data collected by scientists andinstitutions worldwide, edited and merged into a single continuously updatedcompilation of high-resolution seafloor topography.2 ]0 Y; G8 {( a( D* w3 r
$ I7 X# D' G7 j) z8 I4 @7、Plates Boundaries
4 N! u' M/ h: h& h9 J; [6 K
, C$ |2 _8 Z' y/ ~# [9 vWebsite Link 1: http://peterbird.name/oldFTP/PB2002/
8 J7 k5 m. ~0 p) `! x0 v+ v# w& O
8 Q+ C- f7 G5 y( `Source 1 description: Bird,P. [2003] An updated digital model of plateboundaries, Geochemistry Geophysics Geosystems, 4(3), 1027, doi:10.1029/2001GC000252.& c! X, ]; Y0 e
% _0 D0 T, m: UWebsite Link2: www.52ocean.cn
4 A- G, x* S) o" D! [' P; \' U' W: s: w: t- q. K4 R. K
Source 2 description: Alice E. Gripp .[1990] Current plate velocities relative to thehotspots incorporating the NUVEL‐1 global platemotion model .GEOPHYSICAL RESEARCH LETTERS, VOL. 17, NO. 8, P. 1109, doi:10.1029/GL017i008p01109$ `7 }0 z% V. b, {3 |
' A R! P, e) F
8、Centroid-Moment-Tensor(CMT) /Focal Mechanism Solutions(FMS)
' k9 Z4 k% l! U; ~5 D
6 O2 y0 P, f2 b" \Website Link 1: www.52ocean.cn$ \) d% P% m; F5 P
7 s5 S0 @' F; { C
Source 1 description: The Global Centroid-Moment-Tensor (CMT) Project is overseen by Principal Investigator Göran Ekströmand Co-Principal Investigator Meredith Nettles at the Lamont-Doherty EarthObservatory (LDEO) of Columbia University. The project was founded by AdamDziewonski at Harvard University and operated there as the Harvard CMT Projectfrom 1982-2006, led first by Prof. Dziewonski and later by Prof. Ekström.During the summer of 2006, the main activities of the CMT Project moved withProf. Ekström to LDEO. This research effort is moving forward under the name"The Global CMT Project". The main dissemination point forinformation and results from the project is the web site www.52ocean.cn4 p* F0 r4 |, L S( K' ?
' P$ L7 D8 Q9 ?8 l: \- @% SWebsite Link 2: www.52ocean.cn
' P6 M9 j) {5 x5 A3 B
. v' h' d* X: cwww.52ocean.cn (A mirror ofISC in USA, faster access)
2 x+ c* O: x) Z- L/ P* v5 X" l% p2 ~9 w' b
Source 2 description: Web services:International Seismological Centre (ISC) Bulletin: Focal mechanism solutions search3 B* I' K6 K9 f- D- `
0 G% }" o1 W0 T3 J1 r以上资源转自：快乐海洋论坛, S. X5 h1 c! J' P1 t
6 j; P& A4 e7 o; w; Y, D+ Z' o
|
