El Espesor de Springhill (Y) es Función Lineal Y=F(X) de la Paleo-cota (X)

G. Romero

doi:10.3997/2214-4609-pdb.111.47

El Espesor de Springhill (Y) es Función Lineal Y=F(X) de la Paleo-cota (X)
By G. Romero
Publisher: European Association of Geoscientists & Engineers
Source: Conference Proceedings, 9th Simposio Bolivariano - Exploracion Petrolera en las Cuencas Subandinas, Sep 2006, cp-111-00032
DOI: https://doi.org/10.3997/2214-4609-pdb.111.47

Abstract

La Formación Springhill es una unidad sedimentaria transgresiva que se apoya sobre el paleo-relieve<br>volcánico de la Serie Tobífera y subyace a depósitos pelíticos agradacionales. Estas rocas contienen tres<br>markers característicos del perfil de resistividad: los techos de la Serie Tobífera (T1) y de Springhill (S1), y<br>un marker reconocible en la secuencia agradacional (C8).

Article metrics loading...

/content/papers/10.3997/2214-4609-pdb.111.47

2006-09-24

2024-04-24

From This Site

/content/papers/10.3997/2214-4609-pdb.111.47

dcterms_title,dcterms_subject,pub_keyword

-contentType:Journal -contentType:Contributor -contentType:Concept -contentType:Institution

10

5

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.111.47

Most Cited This Month Most Cited RSS feed

- The natural combination of full and image‐based waveform inversion
  
  Authors Tariq Alkhalifah and Zedong Wu
- Poststack diffraction imaging using reverse‐time migration
  
  Authors Ilya Silvestrov, Reda Baina and Evgeny Landa
- Characterizing the effect of elastic interactions on the effective elastic properties of porous, cracked rocks
  
  Authors Luanxiao Zhao, Qiuliang Yao, De‐hua Han, Fuyong Yan and Mosab Nasser
- Fracture detection by Gaussian beam imaging of seismic data and image spectrum analysis
  
  Authors M.I. Protasov, G.V. Reshetova and V.A. Tcheverda
- Laboratory measurements of guided‐wave propagation within a fluid‐saturated fracture
  
  Authors Seiji Nakagawa, Shinichiro Nakashima and Valeri A. Korneev
More Less

El Espesor de Springhill (Y) es Función Lineal Y=F(X) de la Paleo-cota (X)

Abstract

From This Site

Most Read This Month

Most Cited This Month Most Cited RSS feed

The natural combination of full and image‐based waveform inversion

Poststack diffraction imaging using reverse‐time migration

Characterizing the effect of elastic interactions on the effective elastic properties of porous, cracked rocks

Fracture detection by Gaussian beam imaging of seismic data and image spectrum analysis

Laboratory measurements of guided‐wave propagation within a fluid‐saturated fracture