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  Processed seismic data of Cruise SO197 RISE 2008

The aims of cruise SO197 RISE (Rift Processes in the South China Sea) with RV SONNE from Manila, 28th March 2008 to Singapore, 2nd May 2008 are (1) To gain a better understanding of the processes leading to continental breakup and subsequently formation of oceanic crust. (2) To study the evolution of the South China Sea oceanic basin. The South China Sea is particularly well suited for studying rift processes at the transition from extension of continental lithosphere to the formation of oceanic crust. This relatively young marginal basin is currently in a stadium which is characterised by still preserved differences in subsidence and thermal history resulting from rifting. The initial, complex and hardly quantifiable rift processes, however are long enough ago. The area under study comprises the eastern subbasin of the South China Sea, the West Luzon Basin and the transition area from oceanic crust to extended continental crust between the continental blocks of Reed Bank and the islands of Palawan/Calamian Group. By including existing data of earlier cruises (SO-23, -27, -49) a comparison of conjugated margin transects is intended later within the project. A major goal of the project is to study structures at the transition from continental rifting to oceanic spreading and processes resulting from extension of continental lithosphere to the formation of oceanic crust in time and space. The sequence stratigraphy of the synrift and drift sediments will give insights into the formation and evolution of the individual rift basins. The distribution and thickness of the postrift sediments on the continental fragment of the NW Palawan area define the subsidence history. The depth and topography of the Moho show the location of the stretched and thinned crust. By a joint interpretation of the structural setting, the position, distribution and architecture of the basin bounding faults a reasonable rift model will be derived. In addition, we will investigate the transition of a passive rifted margin (off Palawan) to a convergent margin (off Luzon). The timing of the evolution of the South China Sea basin will be more exactly determined by comparing the magnetic anomalies from the eastern subbasin of the South China Sea with existing data from the central/western basin. Particularly the question of a symmetric/asymmetric opening of the oceanic basin and the timing and location of the individual rift/drift episodes will be investigated. Therefore, we investigated rift structures at the southeastern margin of the South China Sea by means of reflection seismology, gravity, magnetics, bathymetry and sediment echosounder and we performed magnetic measurements to identify seafloor spreading anomalies in the eastern subbasin of the South China Sea.
 
Citation proposal
. Processed seismic data of Cruise SO197 RISE 2008. https://gdk.gdi-de.org/geonetwork/srv/api/records/6560d5c6-e881-4206-abbf-2180f68a15e5
 
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  • SDS

INSPIRE

Identification

File identifier
6560d5c6-e881-4206-abbf-2180f68a15e5   XML
Hierarchy level
Dataset
Online resource
Resource identifier
code
7622a094-d258-e9ae-9feb-8fbbd45e70f8
Metadata language
English
Spatial representation type
Vector
Encoding
Format
Shapefile
Version
n/a
Projection
 

Classification of data and services

Topic category
  • Geoscientific information
 

Classification of data and services

Coupled resource
Coupled resource
 
 

Classification of data and services

Coupled resource
Coupled resource
 
 

Keywords

GEMET - INSPIRE themes, version 1.0 ( Theme )
  • Geologie
  • geology
GEMET - Concepts, version 2.4 ( Theme )
  • geophysics
  • Geophysik
  • raw material
  • Rohstoff
Other keywords
Keywords ( Theme )
  • Marine geology
  • Meeresgeologie
  • Seismics
  • Seismik
  • Two-dimensional seismic reflection
  • zweidimensionale Reflektionsseismik
Keywords ( Place )
  • South China Sea
  • Südchinesisches Meer
  • Palawan
  • West Luzon Basin
 
 

Geographic coverage

N
S
E
W


 

Temporal reference

Temporal extent
Temporal extent
Date ( Creation )
2008-05-02
 

Quality and validity

Lineage
In the period from 28th March to 2nd May 2008 BGR acquired seismic lines in the South China Sea and Eastern Archipelagic Seas during cruise SO197 with RV SONNE. All lines BGR08-101 to BGR08-132 are migrated data.
 

Conformity

Conformity
Conformity
 

Conformity

Conformity
Conformity
Explanation
siehe dazu die angegebene Durchführungsbestimmung
 

Restrictions on access and use

Access constraints
Allgemeine Geschäftsbedingungen, siehe http://www.bgr.bund.de/AGB - General terms and conditions, see http://www.bgr.bund.de/AGB_en. Die bereitgestellten Informationen sind bei Weiterverwendung wie folgt zu zitieren: Datenquelle: SO197 RISE 2008, (c) BGR, Hannover, 2019
 

Restrictions on access and use

 

Responsible organization (s)

Contact for the resource
Organisation name
Federal Institute for Geosciences and Natural Resources
Email
Marine_Seismik@bgr.de
 

Responsible organization (s)

Contact for the resource
Organisation name
Federal Institute for Geosciences and Natural Resources
Email
Marine_Seismik@bgr.de
 

Metadata information

Contact for the metadata
Organisation name
Bundesanstalt für Geowissenschaften und Rohstoffe (BGR)
Email
geodatenmanagement@bgr.de
Date stamp
2023-11-16
Metadata language
English
Character set
UTF8
 
 

SDS

Conformance class 1: invocable

Access Point URL
Endpoint URL
Technical specification
 

Conformance class 2: interoperable

Coordinate reference system
 
Quality of Service
 
Access constraints
Limitation
 
Use constraints
Limitation
 
Responsible custodian
Contact for the resource
 
 

Conformance class 3: harmonized

 
 

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6560d5c6-e881-4206-abbf-2180f68a15e5   Access to the portal Read here the full details and access to the data.

  Associated resources

Not available


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